Final Stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar Evidence for Overprinting of the Brasília Belt by the Ribeira Belt Tectonics P

Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Belt Tectonics P. C. Hackspacher Instituto de Geociências e Ciências Exatas, Universidade Estadual Paulista, Av. 24 A, 1515, Rio Claro, SP, CEP 13506-900, Brazil Email: [email protected] A. H. Fetter Instituto de Geociências e Ciências Exatas, Universidade Estadual Paulista, Av. 24 A, 1515, Rio Claro, SP, CEP 13506-900, Brazil W. Teixeira Centro de Pesquisas Geocronológicas, Instituto de Geociências, Universidade de São Paulo, Rua do Lago, 562, São Paulo, SP, CEP 05508-080, Brazil E. L. Dantas Instituto de Geociências, Universidade Federal de Brasília, Brasília, DF, CEP 70910-900, Brazil H. D. Ebert Instituto de Geociências e Ciências Exatas, Universidade Estadual Paulista, Av. 24 A, 1515, Rio Claro, SP, CEP 13506-900, Brazil. R. A. J. Trouw Instituto de Geociências, Universidade Federal do Rio de Janeiro, Cidade Universitária, Ilha do Fundão, Rio de Janeiro, RJ, CEP 21949-900, Brazil. P. Vasconcelos Department of Earth Sciences, University of Queensland, Brisbane, Qld 4072 Australia.

Keywords: Brasiliano orogen, U-Pb, Ar-Ar, Ribeira Belt, Tectonics

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 1 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Abstract: Around the southern margins of the São Francisco Craton, there is a zone of tectonic interference between the Brasília belt to the west and the younger Ribeira belt to the east. U-Pb monazite and 40Ar/39Ar cooling age determinations carried out in the area reveal the cooling histories of these belts and the timing of tectonic overprint, un- raveling the final stages of Brasiliano Orogeny in SE Brazil. The U-Pb monazite data from migmatized paragneisses and late-stage pegmatites in the Socorro-Guaxupé Nappe System of the southern Brasília belt show that migmatization peaked between ca. 613 ±1 and 607±3 Ma. 40Ar/39Ar biotite and muscovite ages of paragneisses and schists in this area indicate that the northern high-grade core of the Nappe System (Guaxupé Do- main) was uplifted and cooled through the 350°C isotherm between 599±1 and 587±1 Ma. In contrast, samples from the southern high-grade core of the Nappe System, the Socorro Domain, south of the Jacutinga shear zone, yields a broader and younger spec- trum of 40Ar/39Ar biotite ages between 571±1 and 562±1 Ma, attributed to a later uplift and cooling of the crust. The cooling ages can be assigned to local resetting of the 40Ar/ 39Ar system during transpressive tectonic overprint due to reactivation as a result of collision of the Ribeira belt. A younger group of 40Ar/39Ar mica ages (537±1 to 521 ±1Ma) in schists of the Socorro Domain, are associated with transpressional structures of the Ribeira belt. Rock samples from the Jacutinga and Três Corações shear zones, yield 40Ar/39Ar biotite-muscovite ages around 520 Ma. These are typical cooling ages of the Ribeira belt, and are interpreted to mark the western limit of the Ribeira belt transpressional regime within the Brasília belt. The youngest biotite-muscovite cooling ages in schists of the Socorro Domain, between 510±2 and 491±1 Ma, mark the final cooling and exhumation of that part of the Brasília belt.

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 2 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 3 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Table of Contents Introduction ...... 5 Geologic Framework ...... 5 Geochronology ...... 8 U-Pb analyses ...... 8 40Ar/39Ar analyses ...... 9 Samples and radiometric results ...... 9 U-Pb results ...... 11 40Ar/39Ar results ...... 13 Discussion and Conclusions ...... 15 Acknowledgements ...... 16 References ...... 16 A. 40Ar/39Ar analytical data ...... 19

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 4 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Introduction of the geology of the belts). The Brasília belt resulted from The Pan-African/Brasiliano Orogeny in South America the closure of the Goianides Ocean (e.g., Pimentel et al., comprises a series of late Neoproterozoic to Cambrian mo- 2000) along the western-southwestern margin of the São bile belts that formed during the assembly of West Gond- Francisco Craton, and merges with the Borborema Prov- wana (e.g., Trompette, 1994). The belts are broadly coeval ince to the north (Fonseca et al., this volume), whereas the in their development, and tectonic aspects. Nevertheless, Ribeira belt is associated with the closure of the Adamastor they are not completely simultaneous; hence structural and Ocean to the east-southeast of the craton (e.g., Campos tectonic interferences related to either thrusting or trans- Neto, 2000). During oceanic closure, subduction gave rise pression exist where they intersect each other. One well- to magmatic arc suites that preceded arc-continent and exposed case of tectonic interaction is in southeastern continent-continent collisions. A sequence of rocks were Brazil where the Ribeira belt transects the Brasília belt, in involved in the amalgamation of West Gondwana includ- the southern margin of the São Francisco Craton. The in- ing: Paleo- and Mesoproterozoic basement rocks and interaction between these two mobile belts during the Brasi- tracratonic successions; Neoproterozoic passive margin liano Orogeny generated a complex array of structures successions; magmatic arcs of intraoceanic and active con- (e.g., Ribeiro et al., 1995; Ebert and Hasui, 1998; Hack- tinental margin settings with pre- and syn-collisional gran- spacher and Godoy, 1999; Campos Neto and Caby, 1999; itoids; late-orogenic sedimentary succession and post Heilbron and Machado, 2003; Valeriano et al., 2004). It is tectonic granites and pegmatites (e.g., Heilbron et al., generally accepted that the final collision of the Ribeira belt 2004). was later than that of the southern Brasília belt (Hasui et The Brasília belt in the region is mainly comprised of a al., 1990; Trouw et al., 2000; Campos Neto and Figueiredo, Neoproterozoic passive margin metasedimentary succes- 1995). However, to what degree the transpressional regime sion (Araxá and Andrelândia Groups), ( Table 1 ). The of the Ribeira belt overprinted the Brasília belt rocks re- Araxá Group comprises quartzite, schist and mafic rocks mains weakly constrained. (Valeriano et al., 2004), whereas the Andrelândia Group Accurate and precise radiometric ages are necessary to contains paragneiss with amphibolite, quartzite, schist, reconstruct the Brasiliano Orogeny and to better under- gondite and calc-silicate rocks (Ribeiro et al., 1995; Pa- stand the regional geologic framework and major structural ciullo et al., 2000). Pimentel et al. (2004a, b) summarized features of each belt. In order to correlate geologic, struc- the evolution of the Brasília belt and its relation to the Goiás tural and geochronologic features of the interference zone, Magmatic Arc ( Table 1 ), as follows: a) formation of in- we present new U-Pb monazite and 40Ar/39Ar mica data traoceanic island arcs, Goiás Magmatic Arc, characterized from selected granitoids, pegmatites, paragneisses and by calc-alkaline volcanic rocks and tonalitic to dioritic plu- schists that crop out in the intersection between the Brasília tons, between 890-800 Ma; b) intrusion of mafic- ultra- belt and central part of the Ribeira belt. These data provide mafic complexes in high metamorphism grade, probably the first detailed age constraints on the late stage of meta- linked to a continental rift environment at ca. 800 Ma; c) morphism, uplift and cooling of the southern Brasília belt, high-grade metamorphism related to collision between the and reveal the thermal and structural overprint of the Ri- northern Goiás Magmatic Arc and the western border of beira belt collision that led to assembly of West Gondwana. the São Francisco proto-craton, between 770-760 Ma (Fer- reira Filho et al., 1994); d) period of igneous quiescence Geologic Framework between 760-680 Ma; e) intrusion of tonalitic, granodioritic, granitic and mafic-ultramafic bodies between 670 and The Neoproterozoic framework of the eastern part of 600 Ma, considered by Junges et al. (2002) as the second the South American Platform comprises mostly older cra- period of generation of tonalites and crustal accretion of tons surrounded by Brasiliano-Pan-African mobile belts the arc; f) peak of metamorphism in the Goías Magmatic (Fig. 1). Convergence between the São Francisco – Congo, Arc associated with the final closure of the Goianides Amazonian and Rio de La Plata Cratons during the assem- Ocean between ca. 630 and 600 Ma (Fischel et al., 1998; bly of West Gondwana generated two major Neoprotero- Pimentel et al., 2000; Piuzana et al., 2002); and g) cooling zoic belts: the Brasília and Ribeira belts (see Cordani et al., and regional uplift between 580-560 Ma (K-Ar, Pimentel 2000; and Heilbron et al., this volume, for a full description et al., 2004b).

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 5 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

In the southern Brasília belt, closer to the Ribeira belt, c. Neoproterozoic units associated to: intra-oceanic arcs the final oceanic closure (point f above) was associated (Adamastor Ocean) and active continental margin set- with the development of significant eastward thrust of tings (790 Ma to 585 Ma), as the Paraíba do Sul, nappes, towards the São Francisco Craton or tangential to Embu, Costeiro and the Oriental Terrane (Rio Negro it (Fig. 1, Table 1; Valeriano et. al, 2004). This Nappe Sys- Magmatic Arc), passive margin and back-arc litho- tem (subdivided into the Guaxupé and Socorro Domains) logical successions and syn-collisional granitoids re- represents a thick Neoproterozoic sheet composed of a pile lated to different collisional episodes; and of high grade metamorphic crustal rocks (Campos Neto and d. post-orogenic sedimentary successions and related bi- Caby, 1999; Campos Neto, 2000). Ages between 611 to modal magmatism of the Cabo Frio Allocthonous 604 Ma in the Socorro and Guaxupé Domains were inter- Terrane (520 Ma; Tupinambá et al., 2000, Heilbron et preted by Trouw and Pankhurst (1993) as a thermal peak al., 2004, and this volume). associated with the earlier thrusting and stacking of the Nappe System. The Socorro-Guaxupé Domains were af- Geochronological studies in the Central Ribeira belt fected by a late- to post-orogenic magmatism between 630 have shown that the closure of the Adamastor Ocean was – 620 Ma (Töpfner, 1996) and 610 – 590 Ma (Janasi et al., a protracted process. The evolution of the Rio Negro Mag- 1993; Ebert et al., 1996; Töpfner, 1996; Wernick, 1998), matic Arc started as early as 790 Ma ago (Heilbron and respectively Numerous NE-trending, dextral, transcurrent- Machado, 2003). The earliest collisional stages followed, transpressive shear zones of the Ribeira belt (Ebert and between 640 to 620 Ma, with west-verging thrusting to- Hasui, 1998) overprint the Brasília belt thrust sheets, par- wards the São Francisco Craton. Sediments of the São ticularly in the southern reworked margin of the São Fran- Roque Group were deposited 610 Ma in a back-arc basin cisco Craton (Fig. 2, Table 1 ). This has also led to relative (Hackspacher et al., 2000). Major collision of the Ribeira vertical displacement of the main Precambrian units of the belt with the Sao Francisco Craton was accompanied by an Ribeira along the Atlantic coast (Hackspacher and Godoy, important tectono-thermal event dated between 590 and 1999; Heilbron et al., 2004). 565 Ma (Machado et al., 1996), interpreted to be associated Figure 2 and Table 1 show the studied area, with di- with thrusting and development of dextral shear zones. In vision of the regional geology into tectonic units: a) the São addition, the tectonic history of the Ribeira belt includes an Francisco Craton, composed of Archean to Paleoprotero- important escape tectonic event, with transpressional char- zoic orthogneisses and migmatitic complexes; b) the Re- acter, juxtaposing different crustal levels (amphibolite and worked Cratonic Border, composed mainly of Archean to greenschist facies), along NE-trending shear zones. This Paleoproterozoic tonalitic and granodioritic orthogneisses, event took place between 600 and 580 Ma ago, as con- strongly reworked during the Neoproterozoic; c) the Bra- strained by U-Pb age of post-kinematic syenitic rocks sília belt and associated Metasedimentary Succession Do- (Töpfner, 1996; Hackspacher and Godoy, 1999). Vertical main (Araxá and Andrelândia Groups), the Guaxupé and movement during this event led to the exhumation of the the Socorro Domains; and d) the Central Ribeira belt (Heil- Brasília and Ribeira belt rocks, with erosion and continen- bron et al., 2004). tal sedimentation in small NE-trending basins developed Like the Brasília belt, the Central Ribeira belt ( Figure between 570-540 Ma (Teixeira et al., 1999; Zanardo and 1 ), across the states of Rio de Janeiro and São Paulo, is a Oliveira, 1990). result of convergence between the São Francisco Craton Subsequent thrusting and development of shear zones and some Neoproterozoic fragments, and the Congo Cra- occurred in the Central Ribeira belt between 535 and 520 ton. Collision processes resulted in the docking of distinct Ma, during the postulated docking of the Cabo Frio terrane tectonostratigraphic terranes, such as (see Heilbron et al., (Schmitt et al., 1999) to the Oriental terrane in the eastern this volume): part of the belt. The late-stage magmatism related to this docking took place between 503 and 492 Ma (Wiedemann a. the Occidental terrane comprised of Paleoproterozoic 1993, Machado et al., 1996, Schmitt et al., 1999). basement rocks; b. Mesoproterozoic volcano-sedimentary successions;

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 6 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Figure 1. Precambrian framework of Western Figure 2. Geologic map of SE Brazil Gondwana

Precambrian framework of Western Gondwana with the Geologic map of SE Brazil (modified after CPRM, 2002) location of the studied area; the southern Brasília belt. with U-Pb and 40Ar/39Ar sample locations and numbers. (modified from Trompette, 1994): 1- Phanerozoic basins; 2- Neoproterozoic Cratons: SF- São Francisco, LA- Luis Alves, RP- Rio de La Plata, C- Congo, K- Ka- lahari; 3- Neoproterozoic mobile belts: B- Brasília, A- Araçuaí, R- Ribeira. Locality: CF: Cabo Frio.

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 7 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Table 1. Tectonic units of the southern Brasília belt Geochronology (Valeriano et al., 2004) and Ribeira belt, as well as the regional shear zones. U-Pb analyses

Geologic Brasília Re- Central Tectonic Initial preparation of monazite crystals for isotopic anal- Period Belt worked Ribeira Process ysis was done at Department of Petrology and Metallogeny Craton Belt State University of São Paulo (UNESP), Brazil. Single 205 235 Border monazite crystals, spiked with a Pb- U tracer solution, were dissolved in 7 ml Teflon Savillex beakers using a sol- Neopro- Jacutinga / Ouro Fino / Trans- ution of concentrated ultra pure H2SO4 (5 uL), 6M HCl terozoic Três Corações shear pression (40 uL) and 7M HNO3 (40 uL). Dissolution of the monazite zones 520 Ma was achieved by placing the beakers on a conventional hot Cabo Frio Collision plate (at 125-140oC) for 24 hours to ensure complete dis- Terrane 520 Ma solution. Samples were then partially dried, as the H2SO4 Jacutinga / Ouro Fino / Trans- is difficult to evaporate, and conditioned with 3.1M HCl Três Corações shear pression prior to microcolumn chromatography, adapted from zones 580-520 Krogh (1973). Isotopic ratios were measured at Geoscience Ma Institute, National University of Brasília (UnB), Brazil, using a Finnigan MAT multi-collector mass spectrometer Costeiro Collision equipped with an ion counting system. Terrane ca. 580 Eleven samples of prismatic monazite were analyzed Ma for both Pb and U isotopic compositions on single Re fil- Passive Margin Sedi- São Ro- Collision aments using silica gel and phosphoric acid. The analyses mentation: Araxa and gue Group ca. 620 were corrected for average mass discrimination of 0.12 ± Andrelania Groups Embu Ma 0.05% per mass unit for multi-collector analyses (based on Terrane replicate analyses of common Pb standard SRM 981). Ura- Granulitic nappes: Occiden- nium fractionation was monitored by replicate analyses of Guaxupe and Socorro tal Ter- SRM U-500. Uncertainties in U-Pb ratios due to uncer- domains rane tainties in fractionation and mass spectrometry were Oriental around ± 0.5%, as all signals measured were relatively Terrane strong. Radiogenic Pb isotopes were calculated by correct- (Rio Ne- ing for modern blank Pb and for original no radiogenic gro Arc) original Pb corresponding to Stacey and Kramers (1975) Paraiba do model Pb for the approximate age of the sample. Uncer- Sul tainties in radiogenic Pb ratios in the studied samples are Goiás 770 Ma typically ± 0.1%. Decay constants and isotopic ratios used Magmatic in the age calculations are those listed by Steiger and Jäger Arc (1977). Total procedure blanks over the course of analyses ranged from 10 to 46 pg for lead and 0.5 to 2 pg for uranium. Meso/Pa- Meso/Pa- Meso/Pa- The U-Pb monazite data (see Table 3 ) were regressed leoproter- leoproter- leoproter- using the ISOPLOT/EX program of Ludwig (1999). For ozoic ozoic ozoic both samples, forced Model 1 regressions were performed Paleopro- Paleopro- Paleopro- as the analytical points were either concordant or nearly terozoic/ terozoic/ terozoic/ concordant with little spread in the data. Uncertainties in Archean Archean Archean concordia intercept ages are given at the 2s level (Fig. 5).

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 8 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

40Ar/39Ar analyses no difference in age can be detected between any two frac- Transmitted- and reflected-light microscopy of polish- tions at the 95% confidence level (Fleck et al., 1977). All ed thin sections were used to determine the mineralogy and uncertainties in plateau, integrated, and weighted mean textures of datable samples. Samples were then crushed ages are given at 2s level. When the plateau ages showed and suitable minerals (well-formed biotite and muscovite comparable individual results within error, the resulting grains) were concentrated and hand-picked under a binoc- age-probability ideogram is taken as a robust estimate of ular microscope. The mineralogical study was conducted the samples’ age (weighted mean age). Figure 3B contains at the Geochronology Laboratory of the State University some examples of weighted mean age corresponding to of São Paulo (USP) and at the Department of Geology of ideograms. Contrastingly, when the plateau ages are sig- the Federal University of Rio de Janeiro (UFRJ), Brazil. nificantly different they indicate a complex thermal history The 40Ar/39Ar geochronology (see Vasconcelos et al., of the sample. In these cases the range between the single 2002) was carried out at the Geochronological Research grain ages has been considered realistic ( Table 4 ; H693C Center (CPGeo) at the University of São Paulo, Brazil. The and HFT361), as additionally supported by the new U-Pb laboratory facility comprises two major units: a home built monazite ages and the regional geochronologic back- fully automated noble gas stainless steel ultra-high vacuum ground. 40 39 gas extraction and purification system, coupled with a con- The Ar/ Ar ages (Ideogram/Integrated) are plotted in tinuous laser, and the MAP-215-50 mass spectrometer. The Fig. 3B which presents the different domains of the Brasília argon routine is limited to grains smaller than 2.1 mm, since and Ribeira belts, north and south of the Jacutinga shear 40 39 this is the maximum diameter of the wells in the sample zone. Figure 6 shows four selected Ar/ Ar analyses for aluminum disks used for irradiation. Five to ten grains from each domain distinguished in the area, whereas Table 4 each sample were loaded into these disks along with Fish presents the age variation of the ideograms for the selected Canyon sanidine standards (28.02 ± 0.28 Ma; Renne et al., group of samples. These ideograms display the thermal 1998). The disks were wrapped in aluminium-foil, sealed history against time within the selected domains. in silica glass tubes and irradiated for 30 hours at the IPEN/ CNEN IEA-R1 nuclear reactor, São Paulo, Brazil. Figure 3. Geologic map of SE Brazil The samples were analyzed after cooling by the laser incremental heating, following procedures detailed by Vas- concelos et al. (2002). Argon isotope ratios (40Ar/39Ar, 38Ar/39Ar, 37Ar/39Ar, 36Ar/39Ar, 40Ar*/39Ar), the percent- age of radiogenic argon (40Ar*), the age obtained for each incremental heating step (identified with a letter after the grain number), J factors, laser beam intensity, 40Ar/36Ar discrimination, correction factors, and full system blanks are shown in the Appendix 1. The calculation of 40Ar/36Ar discrimination (McDougall and Harrison, 1999), was obtained by the measurement of the 40Ar and 36Ar isotopes from the air pipette of the extraction line, in order to ac- Geologic map of SE Brazil (modified after CPRM, 2002) showing: A) U-Pb monazite ages; B) 40Ar/39Ar biotite count correcting factors for the production of interfering and muscovite ages (bold numbers). Symbols as in Fig- isotopes (36Ar, 37Ar, 38Ar, 39Ar, and 40Ar) from Ca and K ure 2. Compare with Fig. 2 for sample numbers. salts and glasses during sample irradiation. Full system blanks correspond to the masses of 40Ar, 39Ar, 38Ar, 37Ar, Samples and radiometric results and 36Ar present in the extraction line and mass spectrom- The timing of late collisional stages of the southern eter. The 40Ar/39Ar incremental heating analyses on three Brasília belt have been derived from U-Pb analyses of single grains from each sample (triplicate analysis) have monazite grains and 40Ar/39Ar analyses of muscovite and provided plateau, ideogram and integrated ages (see Table biotite of high-grade paragneisses, schists, migmatites and 4 ). The plateau ages represent continuous steps (more than late-tectonic pegmatites from the Reworked Cratonic Bor- 50%) of the total 39Ar released from a sample and for which der, Socorro-Guaxupé Nappe System and the

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 9 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Metasedimentary Succession Domains of the Brasília and Figure 4. Field photographs Ribeira belts (Heilbron et al., 2004). Monazite age is used to date peak metamorphism (De Wit et al., 2001; Foster et al., 2004; Gibson et al., 2004; Guillaume-Seydoux et al., 2002) interpreted to be related to the southern Brasília belt evolution, as supported by petrography and field inferen- ces. Ar-Ar is used to date thermal episodes (Noce et al., 2004). All samples studied were taken from locations far from the recognized late sub-vertical shear zones (Jacutinga, Jundiuvira, Camanducaia, São Bento do Sapucaí, Campo do Meio and Três Corações shear zones; Fig. 2) to avoid local tectonic effects. These shear zones are related to the Socorro-Guaxupé Nappe System of the Brasília belt or to the younger escape tectonic at the Central Ribeira belt. Twenty nine samples were analyzed by the 40Ar/39Ar method whilst eleven of them by U-Pb method as well (sample locations and descriptions are in Figs 2, 3 and Table 2 ). U-Pb monazite analyses are summarized in Table 3 , and concordia diagrams are shown in Fig. 5. The 40Ar/39Ar ages are listed in Table 4 , whilst the complete analytical data are shown in Appendix 1. Four plots of the 40Ar/39Ar dates illustrate the history of uplift and cooling for the studied domains (Fig. 6A-D). Field photographs. A) Paragranulite of the Guaxupé Do- main, sample H693; B to D) paragneisses of the Socorro Domain (samples HFT353, HFT349, H704 respectively); E) Schist interlayered with quartzites of the Metase- dimentary Succession Domain, sample H687.

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 10 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Table 2. Sample Description U-Pb results Sample Lithology Prove- Coordi- Analysis The oldest populations of monazite were found in the nance nates Guaxupé Domain. U-Pb age determinations of monazite grains from a single sample of migmatite (HFT 359, Figs Guaxupé Domain 3A, 5A and Table 3) yield a discordant age of around 642 HFT359 Banded, road be- 21º 42' gneissic ±1 Ma. This age represents an early generation of monazite biotite tween Po- 0.6"S, 46º banding growth related to an early metamorphic event. This event paragneiss ços and 22' 56"W (122/09) is roughly contemporaneous to that in the Socorro Domain, Machado composed associated with the pre-collisional granites of Hackspacher Minas of narrow et al. (2003). Gerais bands of State- MG quartz, Figure 5a. U-Pb concordia diagrams plagio- clase, biotite , K- feldspar and prismatic monazite crystals HFT361 Augen road be- 21º 42' gneissic gneiss tween Ma- 52"S, 45º banding chado and 55' 35"W (80/10) Pouso and thrust Alegre- sense to MG west composed by K-feldspar por- phyro- blasts in a quartz- feldspath- ic matrix, biotite and

well U-Pb concordia diagrams of monazite data from para- formed gneisses. migmatites and pegmatites in the southern monazite part of the: Brasília belt, Guaxupé Domain: as acces- a. HFT359 sory min- b. HFT361 eral c. H693A. d. Socorro Domain: H616, H693 Paragra- road Var- 21º 33' gneissic e. FCS-11B, nulite ginha- 25"S, 45º banding f. HFT353B, (Fig. 4A) Carmo 22' 07"W (232/11) alternat- Ca- and ing with choeira- stretching kinzigite MG, at the lineation and meta- Santo An- (252/8) Final stages of basitethe Brasiliano tônioOrogenesis in SE Brazil: U-Pbwith and trans- 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 11 Belt Tectonics quarry port sense to north- east. It is composed by K-feldspar, garnet, kyan- ite and hy- persthene, biotite and prismatic monazite H465 Schist al- road be- 21º 22' foliation ternating tween Par- 51"S, 45º (172/12) with aguaçu 30' 20"W composed quartzite and Vargi- by quartz, and granu- nha-MG biotite and litic gneiss K-feldspar H559 Schist in- road 381 21º 33' foliation tercalated between 37"S, 45º (212/15). with Três Cora- 08' 16"W It is com- quartzite ções and posed by and calc- Carmo da quartz, bi- silicate Ca- otite, K- choeira- feldspar MG and muscovite H690 Schist , road Cam- 21º 45' foliation. gneiss and buquira- 21"S, 45º It is com- amphibo- Três Cora- 14' 18"W posed by lite ções-MG bands of quartz, K- feldspar, plagio- clase and biotite . Amphibo- lite boudins are stretched along the main banding Socorro Domain H616 Pegmatite road be- 22º gneissic cutting a tween Ita- 23'54''S, banding migmatit- jubá and 45º (175/10) ic para- Pedralva- 32'00''W and gneiss MG stretching lineation (182/8) with trans- port sense to north, composed by K-feldspar, pla- gioclase, biotite and prismatic monazite ; FCS11B Pegmatite road be- 23º Granitoid cutting tween 17'53''S, with an granitoid Jundiaí 47º equigra- and Itu-SP 02'60''W nular tex- ture composed by quartz, plagio- clase, biotite and K- feldspar, and prismatic monazite crystals HFT353B Para- road be- 22º 31' gneissic gneiss tween 23"S, 46º banding (Fig. 4B) Cambuí 01' 25"W (105/08), with mig- and Pouso composed matitic Alegre- by bands features MG of K–feldspar, pla- gioclase, biotite and garnet crosscut by quartz- feldspath- ic pegmatite. The sample shows prismatic monazite prismatic biotite grains. HFT349 Para- road be- 22º 44' gneissic gneiss tween São 29"S, 45º banding (Fig. 4C) Bento do 44' 21"W (117/11) and schist Sapucaí and asym- and Parai- metric iso- sópolis- clinal fold MG with axis plunging 5 degrees to NNE and foliation parallel to banding, composed by narrow bands of quartz, plagio- clase, biotite, K- feldspar and garnet. The sample yielded some prismatic monazite and biotite grains H751 Schist , road be- 22º 38' foliation paragneiss tween Sa- 34"S, 45º (147/52) and mig- pucaí- 44' 58"W composed matite Mirim and by quartz, São Bento K-feld- do Sapu- spar, bio- caí-MG tite and muscovite. The sample yielded prismatic biotite grains. HFT704B Pegmatite road SP 65 23º gneissic (Fig. 4D) between 10'15''S, banding related to Bom Jesus 46º 23' (137/43) intrusive dos Per- 24''W with granite dões and stretching and or- Nazaré lineation thogneiss Paulista- (135/40) SP and NW sense of thrusting. The or- thogneiss is composed by plagio- clase, K- feldspar, biotite and is intruded by granite with K- feldspar, plagio- clase and biotite. The sample yielded well- formed monazite grains. H355 Augen road Bom 22º 22' gneissic gneiss Repouso 06"S, 46º banding to Borda 08' 30"W (123/13), da Mata- composed MG by K-feldspar pro- phyro- blast in a quartz- feldspath- ic matrix. The sample yielded well- formed biotite grains H351 Para- road be- 22º 32' gneissic gneiss tween Par- 34"S, 45º banding aisópolis 50' 38"W composed and Con- by small solação- bands of MG quartz, plagio- clase, biotite and K- feldspar Reworked Cratonic Border HFT363B Pegmatit- Sindicato 22º 16' banding ic veins quarry at 45"S, 46º (137/05), cutting the road 10' 55"W composed paragneiss between by bands with mig- Borda da of quartz, matitic Mata and plagio- features Ourofino- clase, bio- MG tite and K- feldspar and quartz- feldspath- ic pegmatite. Am- phibolite boudins are stretched along the main banding. Biotite , muscovite and rare monazite crystals are well preserved H681 Para- road Pou- 22º 05' gneissic gneiss so Alegre- 35"S, 45º banding with mig- Silvianóp- 53' 32"W (225/20) matitic olis-MG and portions stretching lineation (230/70), composed by K-feldspar, pla- gioclase, biotite and garnet. The sample present well formed biotite and monazite crystals HFT358 Granitoid road be- 22º 05' equigra- (syn to tween 59"S, 46º nular tex- post-tec- Borda da 10' 57"W ture com- tonic) Mata and posed by Ipuíuna- quartz, MG plagio- clase, biotite and K- feldspar. The sample present well formed biotite crystals HFT356 Schist in- road be- 21º 03' foliation tercalating tween Ja- 03"S, 46º ( 172/74) with cutinga 08' 37"W composed gneiss and and Ouro- by quartz, migmatite fino-MG biotite, K- feldspar and muscovite Metasedimentary Sucession Domain H687 Pegmatite road Cam- 21º 53' foliation cutting buquira- 29"S, 45º (340/10) metasse- Lambari- 15' 46"W and diments MG stretching (Fig. 4E) lineation in am- (64/00), phibolite composed facies by K-feldspar, quartz, muscovite and biotite crystals; The sample present well formed biotite and muscovite crystals LUME Schist , road be- 21º 33' foliation quartzite tween Lu- 30"S, 44º ( 272/15) and meta- minárias 57' 15"W composed conglom- and Lav- by quartz, erate of ras-MG muscovite the Andre- and bio- lândia tite. The Group sample yielded prismatic muscovite crystals ITMTR Schist , road be- 21º 21' foliation quartzite tween Lu- 00"S, 44º (179/13) and meta- minárias 52' 00"W composed conglom- and Lav- by quartz, erate of ras-MG muscovite the Andre- and bio- lândia tite. The Group sample yielded prismatic muscovite crystals MN85 Schist , road be- 21º 40' foliation quartzite tween 20"S, 44º (269/10) and meta- Três Cora- 57' 34"W composed conglom- ções and by quartz, erate of São Bento muscovite the Andre- do Abade- and biotite lândia MG Group MR72 Schist and road be- 21º 40' foliation quartzite tween São 20"S, 44º (280/12) of the An- Bento do 57' 00"W composed drelândia Abade and by quartz, Group Luminá- muscovite rias-MG and biotite CAR1 Schist , road be- 21º 27' foliation quartzite tween São 00"S, 44º ( 315/35) and meta- João Del 34' 00"W composed conglom- Rei and by quartz, erate of São Tia- muscovite the Andre- go-MG and biotite lândia Group DIT Schist and road be- 21º 33' foliation quartzite tween 00"S, 44º (137/17) of the An- Lavras 24' 45"W composed drelândia and São by quartz, Group João Del muscovite Rei-MG and biotite ANDT Schist , road be- 21º 45' foliation quartzite tween Ma- 00"S, 44º (142/23) and meta- dre de 18' 00"W composed conglom- Deus de by quartz, erate of Minas e muscovite the Andre- Andrelân- and biotite lândia dia-MG Group FDA Schist , road be- 21º foliation quartzite tween Ma- 52'15''S, (133/15) and meta- dre de 44º composed conglom- Deus de 15'35''W by quartz, erate of Minas e muscovite the Andre- Andrelân- and biotite lândia dia-MG Group Ribeira belt H513B Pegmatite at Ibiúna- 23º 43' equigra- cutting SP 53''S; 47º nular tex- syntecton- 24' 26''W ture com- ic granite posed by quartz, plagio- clase, biotite and K- feldspar, and well formed monazite crystals H109 Schist , road 21º 33' foliation paragneiss BR-116 37"S, 45º (177/45) and mig- between 08' 16" W composed matite Itatiaia by quartz, and Re- biotite , K- sende-RJ feldspar and muscovite Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Figure 5b. U-Pb concordia diagrams granites, which may have re-homogenized the monazite ages of older migmatites and paragneisses. One sample of pegmatite was dated. Pegmatites are mostly undeformed except for local boudinage and are interpreted to be late tectonic. They are intrusive into garnet- schists of the Andrelândia Group (Metasedimentary Succession Domain), in the southern edge of the Brasília belt. This monazite sample yielded an almost concordant U-Pb age of 598±2 Ma (Fig. 5I, sample HFT363B).

U-Pb concordia diagrams of monazite data from paragneisses. migmatites and pegmatites in the southern part of the: Brasília belt, Guaxupé Domain:

g. HFT349, h. H704B. i. Reworked Cratonic Border: HFT363B, j. H681. k. Ribeira belt: H513B.

Granulites, migmatites and paragneiss leucosomes of both the Guaxupé and Socorro Domains (Brasília belt) yield concordant ages between of 620±2 Ma, sample HFT 359, Guaxupé Domain, and 625±1 Ma, sample H616, So- corro Domain (Figs 3A, 5D and Table 3). Nearly concordant U-Pb monazite ages between 613 and 607 Ma were also found (samples H693A, H361, FCS 11B, HFT 353, H 704, H 681, H513B in Figure 3 a, Figure 4 , Figure 5a and Table 3 ). Geological and textural evidence, such as monazite inclusions in garnet, suggest that these old monazite grains grew during peak metamorphism (e.g., De Wit et al., 2001; Foster et al., 2004; Gibson et al., 2004; Guillaume- Seydoux et al., 2002). In the Brasília belt these early- formed monazite grains were found in high-grade rocks associated with low angle shear zones, syn-collisional

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 12 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Table 3. U-Pb monazite data from the southern Brasília 40Ar/39Ar results belt The study of monazite growth ages marking thermal S P P ± P ± C P ± P ± P ± P ± peak is complemented by the study of Ar-Ar cooling ages. a b b b o b b b b This thermochronometer was used here to identify the m 2 2 2 r 2 2 2 2 overprinting of the Ribeira belt deformation on the Brasília pl 0 0 0 r 0 0 0 0 belt. In the northern portion of the Nappe System, north of 40 e 6 7 6 el 7 6 7 7 the Jacutinga shear zone, in the Guaxupé Domain, Ar/ 39 * * . * * * * Ar data from biotite (Group 1 in Table 4 , Figure 3 B), yield a fairly tight cluster of cooling ages (plateau and ide- F W U P P U 2 U 2 C P 2 U 2 U 2 P 2 ogram), between 599±1 and 587±3 Ma (Fig. 6A, sample r t. b b 2 σ 2 σ o b σ 2 σ 2 σ b σ HFT465). Muscovite sample (H559: 588±2 Ma) yields a 2 3 3 ef 2 3 3 2 similar ages to biotite. This indicates that the northern part ct 0 5 8 f. 0 8 5 0 of the Nappe System cooled to ~350 oC some 20-30 myr io 4 6 6 after peak metamorphism. n * * In the southern portion of the Nappe System, south of ( p p ( % % ( % A ( A ( A ( the Jacutinga shear zone, 40Ar/39Ar biotite data show a m p p o r g M g M g M varied cooling history. The oldest ideogram biotite ages g) m m b h e a) e a) e a) yielded a value of 597±1 Ma (sample HFT355), similar to s. o) the northern part of the Nappe System, and interpreted to ) represent a relict of that cooling phase. The next oldest G sample obtained in this region is younger, ranging between u 571±1 to 566±1 Ma (Group 2 in Table 4, Figs 3B, 6B sam- a ple HFT358), and include muscovite age between 566-562 x Ma (Group 2 in Table 4 , sample HFT356). u A third group of samples south of the Jacutinga shear p zone is associated with transpressional structures of the é Central Ribeira belt, such as the NE-SW trending sub ver- D tical strike-slip Jacutinga and Três Corações shear zones, o which separate the Guaxupé and Socorro Domains. They 40 39 m yield Ar/ Ar biotite ideogram ages from 527±1 to 521 ±1 Ma (Group 3 in Table 4, e.g. samples HFT353 H681 ai and LUME, Figs 3B, 6C). The 40Ar/39Ar systematics in this n area has been perturbed, as indicated by age spectra of the H sample H687B that vary from 557±2 to 527±1 Ma. The F youngest group of ages south of the Jacutinga shear zone T yield biotite/muscovite ideogram ages from 510±2 to 491 3 ±1Ma (group 4 in Table 4, Figs 3B and 6D sample FDA). 5 Six 40Ar/39Ar cooling age determinations in the eastern 9 sector, near the boundary to the Ribeira Belt, show an age M 0. 4 2 1 0. 0. 0. 0. 0. 0. 0. 6 2 6 2 6 1 distribution between 501±2 and 491±1 Ma (see for exam- (0 0 6 4 2 8 2 1 2 9 0 0 2 2 4 ple FDA, ANDT in Table 4). . 1 4 5 4 5 8 0 7 7 6 6 4 8 2 Thus, the age patterns in the Nappe System south of the 4 8 3 9 9 6 1 4 1 Jacutinga shear zone (Groups 2, 3 and 4), show that group A 6 4 7 0 3 samples from the Jacutinga and Três Corações shear )2 8 zones are younger than elsewhere (group 2), while group M 0. 1 6 1 0. 0. 0. 0. 0. 0. 0. 6 2 6 2 6 1 4 probably reflects a new tectonic event. Their geographi- (0 0 3 8 8 8 3 1 3 9 0 0 2 2 2 cal distribution, closer to the Ribeira belt boundary, . 1 3 1 4 4 2 0 2 9 6 3 0 0 0 5 8 5 1 6 2 1 4 0 Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 13 BeltA Tectonics7 1 3 0 4 )2 7 H F T 3 6 1 M 0. 6 1 1 0. 0. 0. 0. 0. 0. 0. 6 5 6 4 6 1 (0 0 5 1 1 8 9 0 7 7 0 5 0 1 4 2 . 1 2 1 7 2 0 9 1 8 6 5 4 2 4 5 4 3 0 7 8 5 1 A 6 2 1 )2 4 M 0. 6 1 1 0. 1. 0. 0. 0. 0. 1. 6 7 6 3 6 2 (0 0 8 4 4 8 1 0 5 4 0 0 0 0 0 3 . 1 8 4 7 2 9 9 5 7 6 5 9 8 7 5 2 9 1 0 9 3 0 A 7 0 1 )4 0 H 6 9 3 A M 0. 1 1 7 0. 0. 0. 0. 0. 0. 0. 6 3 6 3 6 2 (0 0 9 7 3 8 5 0 5 9 0 0 1 1 1 . 3 6 2 7 2 4 9 3 9 6 8 2 2 1 5 0 2 2 1 7 9 0 0 A 1 6 2 )3 1 M 0. 3 2 7 0. 0. 0. 0. 0. 0. 0. 6 4 6 4 6 5 (0 0 5 0 5 8 7 0 6 9 0 2 1 1 1 . 2 5 7 3 2 2 9 8 3 6 5 2 2 1 5 0 1 5 9 7 9 8 0 A 1 7 1 )4 9 S o c o rr o D o m ai n H 6 1 6 M 0. 2 1 2 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 1 (0 0 6 2 0 8 1 1 1 9 0 0 2 2 2 . 0 2 0 2 5 9 0 8 5 6 6 6 5 0 5 9 3 7 7 0 2 5 0 A 1 2 0 4 ) 4 M 0. 2 9 1 0. 0. 0. 0. 0. 0. 0. 6 2 6 2 6 1 (0 0 3 4 6 8 2 1 2 9 0 0 2 2 2 . 1 7 2 7 5 8 0 7 7 6 7 6 5 1 5 2 7 4 0 2 2 0 5 8 6 0 4 A 8 ) M 0. 1 1 8 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 1 (0 0 7 1 3 8 2 1 2 9 0 0 2 2 1 . 1 3 9 4 4 1 0 1 6 6 6 6 4 5 6 1 9 1 1 8 2 0 0 A 4 0 3 ) 2 F C S 1 1 B M 0. 4 1 2 0. 0. 0. 0. 0. 0. 0. 5 5 6 5 6 2 (0 0 4 5 5 8 7 0 7 9 0 0 9 0 1 . 0 8 7 5 0 6 9 5 9 6 9 8 1 1 3 8 2 1 4 6 7 3 0 A 9 2 2 )" 1 1 " M 0. 7 2 2 0. 0. 0. 0. 0. 0. 0. 6 3 6 3 6 2 (0 0 2 5 6 8 4 0 4 9 0 0 0 0 0 . 0 1 8 1 0 7 9 6 8 6 9 1 2 8 3 6 8 0 1 9 7 0 0 A 8 7 1 )" 1 2 " M 0. 2 1 2 0. 0. 0. 0. 0. 0. 0. 6 3 6 3 6 4 (0 0 5 0 9 8 5 0 5 9 0 1 0 0 1 . 0 5 5 4 1 6 9 3 5 6 7 5 7 5 3 8 2 1 7 8 8 1 0 A 5 4 3 )" 3 3 " H F T 3 5 3 B M 0. 1 1 2 0. 0. 0. 0. 0. 0. 0. 6 2 6 2 6 4 (0 0 5 0 1 8 3 0 3 8 0 1 0 0 1 . 1 7 3 4 1 9 9 3 6 6 9 5 6 2 4 0 4 5 9 7 8 8 0 A 6 4 2 )1 5 M 0. 1 1 3 0. 0. 0. 0. 0. 0. 0. 5 2 6 2 6 5 (0 0 2 1 5 8 3 0 3 8 0 2 9 0 1 . 2 3 8 6 0 7 9 1 6 1 9 2 1 4 4 5 4 1 8 7 4 0 A 7 4 2 )2 0 M 0. 9 9 3 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 3 (0 0 0 7 4 8 2 0 2 8 0 1 0 0 1 . 2 0 7 0 1 5 9 2 6 4 3 5 1 5 8 0 3 8 8 0 A 7 0 2 )2 0 H F T 3 4 9 M 0. 2 1 3 0. 0. 0. 0. 0. 0. 0. 5 4 5 4 6 3 (0 0 2 2 4 8 6 0 6 9 0 1 9 9 0 . 2 3 7 5 0 4 9 3 8 6 3 7 9 6 4 8 4 1 3 3 7 0 0 A 6 0 0 )2 6 M 0. 5 1 1 0. 0. 0. 0. 0. 0. 0. 6 3 6 3 6 1 (0 0 0 5 3 8 4 0 4 9 0 0 0 0 1 . 2 6 6 3 1 6 9 5 9 6 5 4 6 3 5 6 1 4 9 6 8 3 0 A 0 5 3 2 )2 7 H 7 0 4 B M 0. 2 8 1 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 1 (0 0 2 1 3 8 1 0 1 9 0 0 0 0 0 . 0 8 0 6 1 7 9 7 8 6 3 8 8 8 6 8 2 6 9 8 8 0 A 2 7 9 1 ) 2 M 0. 1 6 2 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 1 (0 0 8 4 2 8 2 0 2 9 0 0 1 0 0 . 1 0 0 3 2 1 9 6 6 6 0 9 6 6 2 8 9 1 9 3 0 5 3 5 2 0 A 7 ) M 0. 1 1 1 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 1 (0 0 6 0 6 8 1 1 1 9 0 0 2 2 0 . 1 8 0 5 4 9 0 8 5 6 6 5 1 9 7 5 4 2 9 3 1 7 0 0 4 9 7 1 A 6 ) R e w o rk e d C r at o ni c B o r d er H F T 3 6 3 B M 0. 1 3 5 0. 0. 0. 0. 0. 0. 0. 5 4 5 4 6 2 (0 0 6 1 5 8 6 0 6 9 0 0 9 9 0 . 2 6 9 4 0 7 9 6 9 5 9 7 8 1 4 0 8 4 5 2 7 2 9 A 5 2 1 9 )2 3 M 0. 9 2 8 0. 1. 0. 1. 0. 0. 0. 5 8 5 8 6 3 (0 0 9 1 0 7 2 0 2 9 0 1 9 9 1 . 2 1 0 2 9 8 9 7 9 6 5 2 6 0 5 6 9 9 6 8 6 4 0 A 3 2 1 )2 7 H 6 8 1 M 0. 1 4 1 0. 0. 0. 0. 0. 0. 0. 6 3 6 3 6 2 (0 0 1 9 6 8 5 0 4 9 0 0 0 0 0 . 2 8 1 5 1 0 9 9 8 6 9 4 5 9 3 6 4 7 4 8 5 0 A 6 2 1 ) 6 M 0. 1 4 2 0. 0. 0. 0. 0. 0. 0. 6 5 6 5 6 1 (0 0 2 5 0 8 7 0 5 7 0 2 0 0 0 1 . 0 8 2 7 1 9 9 7 4 6 3 3 4 7 5 9 4 4 3 8 5 0 A 1 1 1 ) 0 R ib ei r a B el t H 5 1 3 B M 0. 9 1 1 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 1 (0 0 8 2 6 8 1 0 1 9 0 0 1 1 0 . 1 9 1 4 2 7 9 6 5 6 5 1 0 5 3 0 4 5 3 9 3 0 A 4 5 0 )" 4 1 " M 0. 1 7 2 0. 0. 0. 0. 0. 0. 0. 6 1 6 1 6 1 (0 0 4 0 7 8 2 0 2 9 0 0 0 0 0 . 1 6 2 3 1 1 9 1 9 6 2 9 8 4 3 0 5 7 9 9 4 0 A 3 0 0 )" 2 2 " M 0. 1 9 9 0. 0. 0. 0. 0. 0. 0. 6 2 6 2 6 3 (0 0 1 7 2 8 3 0 3 9 0 1 0 0 0 . 0 3 8 7 1 6 9 4 4 6 2 7 7 7 3 4 0 8 8 7 0 A 5 8 1 )" 0 3 " Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/ suggests a possible late overprint. The cooling ages of Table 4. 40Ar-39Ar data (single grains; triplicate) from groups 3 and 4 are interpreted to have been reset by motion the southern Brasília belt. See Table 2 for sample on vertical shear zones south of the Jacutinga and Três details. Errors are given in 2s. Corações shear zones producing a range of younger ages. Sam- Rock Lab # Pla- Pla- Pla- Ideo- Inte- Figure 6. Incremental heating analysis of single grains ple /Min- teau 1 teau 2 teau 3 gram grat- eral ed USP Ages Ages Ages Ages Ages (Ma) (Ma) (Ma) (Ma) (Ma) Grou p 1- North of Ja- cutinga shear zone: north ern part 40Ar/39Ar incremental heating analysis of single grains of the with plateau ideogram and integrated graphics. So- a. North of Jacutinga shear zone, sample HFT 465. cor- View Figure 6a [fullsize] (above). ro- b. South of the Jacutinga shear zone, sample HFT Guax 358. View Figure 6b [fullsize]. c. South of Jacutinga shear zone, sample HFT 353. upé View Figure 6c [fullsize]. do- d. South of Jacutinga shear zone, sample FDA. View mains Figure 6d [fullsize]. HFT3 para- 1512 601 598 598 599 See Table 4 for details. 59 gneis ±1 ±1 ±1 ±1 s/biotite HFT3 augen 1513 588 586 591 584 61 gneis ±1 ±1 ±1 ±1 s/biotite H693 para- 1485 574 578 586 579 C gran- ±1 ±1 ±1 ±1 ulite/ biotite H465 schist 1489 586 589 585 587 /bio- ±1 ±1 ±1 ±1 tite H559 schist 1491 591 587 587 588 /mus- ±1 ±1 ±1 ±2 covite Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 14 Belt Tectonics Grou p 2- South of Ja- cutinga shear zone HFT3 augen 1507 597 599 597 597 55 gneis ±1 ±1 ±1 ±1 s/biotite HFT3 para- 1494 572 570 572 571 49 gneis ±1 ±1 ±1 ±1 s/biotite HFT3 para- 1495 567 575 543 560 51 gneis ±2 ±1 ±1 ±1 s/biotite HFT3 schist 1509 567 566 567 566 56 /mus- ±1 ±1 ±1 ±1 covite HFT3 gran- 1510 568 568 555 568 58 itoid/ ±1 ±1 ±1 ±1 biotite Grou p 3- South of Ja- cutinga shear zone (hy- brid ages) HFT3 para- 1506 537 535 540 537 53B gneis ±1 ±1 ±1 ±1 s/biotite HFT3 peg- 1515 538 537 525 537 63B mat- ±1 ±1 ±1 ±1 ite/biotite HFT3 peg- 1516 562 561 562 562 63B mat- ±1 ±1 ±1 ±1 ite/ muscovite CAR schist 927 525 536 521 526 1 /mus- ±1 ±3 ±2 ±3 covite H687 peg- 1501 557 527 541 533 B mat- ±2 ±1 ±1 ±1 ite/biotite H687 peg- 1502 528 539 535 533 B mat- ±1 ±1 ±1 ±2 ite/ muscovite H690 schist 1503 534 546 544 541 /bio- ±1 ±1 ±1 ±1 tite LUM schist 922 531 526 511 527 E /mus- ±2 ±1 ±2 ±4 covite MN8 schist 929 553 545 523 537 5 /mus- ±2 ±2 ±1 ±2 covite H681 para- 1499 521 522 518 521 gneis ±1 ±1 ±1 ±1 s/biotite Grou p 4- South of Ja- cutinga shear zone H109 schist 1488 492 490 492 491 /bio- ±1 ±1 ±1 ±1 tite H751 schist 1492 516 514 524 518 /bio- ±1 ±1 ±1 ±1 tite MR7 schist 928 bad 512 509 510 2 /mus- run ±1 ±2 ±2 covite AND schist 921 499 504 501 501 T /mus- ±1 ±1 ±1 ±2 covite DIT schist 919 497 497 493 494 /bio- ±1 ±1 ±1 ±3 tite DIT schist 918 499 494 500 498 /mus- ±2 ±2 ±1 ±2 covite FDA schist 932 501 501 501 501 /bio- ±1 ±1 ±1 ±1 tite FDA schist 931 502 496 495 496 /mus- ±2 ±1 ±1 ±1 covite ITM schist 924 500 506 507 503 TR /mus- ±1 ±1 ±2 ±2 covite Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Discussion and Conclusions Figure 7. Biotite and muscovite age-histogram The U-Pb and 40Ar/39Ar ages presented above can be divided into different groups which define the tectonic history of different blocks related to the collision and amalgamation of the Neoproterozoic around the southern limit of the São Francisco Craton. These final stages occur at different times and overprint differently the Brasília and Ribeira belts ( Figure 7 ). The older U-Pb monazite ages between 642±1 and 620±1 Ma (H359) from migmatites and high-grade paragneisses of the Guaxupé Domain in the southern Brasília belt, are considered to date the main met- U-Pb monazite and 40Ar/39Ar biotite and muscovite age- amorphic phase associated with granitic plutonism, colli- histogram of the Southern Brasília and Central Ribeira sion and a tangential tectonic regime ( Figure 7 ). This is belts. See text for details. supported by U-Pb data and geologic constraints from the The 40Ar/39Ar ages in the range between 580 – 520 Ma, Socorro Domain indicating pre- to syn-collisional process- defining groups 2 and 3, include rocks south of the Jacu- es between 650 and 628 Ma (Hackspacher et al., 2003; tinga shear zone (Socorro Domain) and reflect a complex Piuzana et al., 2002; Pimentel et al., 2004). history of exhumation of the Nappe System. Transpres- The U-Pb monazite ages from the Guaxupé and Socorro sional structures in the Brasília belt characterize deforma- Domains between 613±1 and 607±3 Ma represent late tion during this time and are interpreted to be related to the stage metamorphism of the Brasília belt associated with tectonic evolution of the Central Ribeira belt ( Figure 7 ) eastward thrusting and nappe stacking. Pegmatites intrud- as described in the regional geology. At that time the main ing upper crustal level have concordant monazite ages of tectonic activity in the Ribeira belt changed from a com- around 598 Ma (Fig. 5I). They were associated with the pressive to an extensional regime where ductile shear zones final magmatic evolution, popossibly the same event re- evolved to brittle systems. ported by Janasi et al. (2001) in the Guaxupé Domain, In the Socorro Domain, the 40Ar/39Ar ages from 571±1 between ca. 610 and 580 Ma. This late magmatism is in- and 560±1 Ma down to 537±1 and 521±1 Ma, are signifi- terpreted to represent the post-orogenic uplift of the Bra- cantly younger than those north of the shear zone. This sília belt (Wernick, 1998) and marks the final closure of delayed cooling reflects either different times of exhuma- the Goianides Ocean (Fischel et al., 1998; Pimentel et al., tion, or partial resetting due to reheating during transpres- 2000; Piuzana et al., 2002). Magmatic ages between 595 sional tectonics related to the Ribeira belt. Supported by a and 560 Ma record the main period of tectonic activity in component of vertical displacement along the strike-slip the Ribeira belt (Machado et al., 1996) suggesting that shear zones, and contrasting metamorphic conditions on magmatism in the easternmost part of the Brasília belt either side of Jacutinga shear zone (greenschist and am- could be a response to tectonic and possibly magmatic ac- phibolite facies), we favour a later exhumation for this tivity in the Central Ribeira belt. Biotite 40Ar/39Ar cooling domain, but further interpret the variability of apparent ages of 599±1 and 587±1 Ma from the paragneisses of the ages of single samples as representing overprinting by tec- Guaxupé Domain indicate that the nappe system cooled tonic activity related to the Ribeira belt. The apparent from the 700 oC closure temperature of monazite to 350 cooling ages around 520 Ma from samples located along oC over 10-20 myr, possibly as a result of exhumation of the NE-SW trending sub-vertical strike-slip Jacutinga and the southern Brasília belt. Três Corações shear zones between the Guaxupé and So- corro Domains (Fig. 3) define both the latest time and the westernmost limit of the effects of the Ribeira belt tectonic on the Brasília belt. The youngest group of 40Ar/39Ar ages, between 505 and 490 Ma, is limited to the Metasedimen- tary Succession Domain (see Fig. 3A-B), south of the Jacutinga shear zone, are identical to typical cooling ages

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 15 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/ in the Ribeira belt along the Atlantic coast further to the belt and subsequent transpression. This late event caused east. Thus, we interpret these ages to reflect final uplift. the resetting of cooling ages to between 580 and 520 Ma. The 40Ar/39Ar cooling ages of samples ANDT, DIT, Late cooling ages recorded by samples from the Jacutinga FDA, ITM TR and TI45 (Group 4, Table 4 ) are the young- shear zone marks the northwestern limit of a progressive est and suggest a trend ageing to the NW within the regional cooling, associated to the Ribeira belt transpres- Metasedimentary Succession Domain. Although more data sional tectonics. is required to establish this trend, the data suggest progressive partial reheating related to exhumation of the Central Acknowledgements Ribeira belt. The authors are grateful for support provided by FA- 40 39 In summary, integration of U-Pb and Ar/ Ar ages, PESP (grant numbers 96/4403-5, 97/06544-8, 97/1397-7, supported by geologic documentation, indicates that the 93/4550-0, 01/04420 –7, 99/00358-3 and 00/03960-5) and southern Brasília belt was reactivated by the younger Cen- CNPq (grant numbers 52.2388/95-7, 400490/94-3, tral Ribeira belt. Such interaction took place from the end 522386/95-4) to make this research possible, and to Artur of the Neoproterozoic to early Phanerozoic, during the as- Takashi Onoe of the Institute of Geosciences at USP for sembly of West Gondwana. The southern margins of the analyzing the 40Ar/39Ar samples for this study and to Dan- Brasília belt reached the main collision phase with the São iel Godoy and Marli C. Ribeiro of the Institute of Geo- Francisco Craton at 620 Ma ( Table 1 ) and peak metamor- sciences at UNESP for drafting the figures. We thank phism at 610-590 Ma as indicated by monazite ages. This Robert Ancskiewicz, Bruce Schaefer and Roberto Wein- was followed by exhumation and cooling before a late berg for detailed and careful review. overprinting as a result of collision with the Central Ribeira

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 16 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

References Guillaume-Seydoux, A, Paquette, J. L., Wiedenbeck, M, Montel, J. M. and Heinrich, W., 2002. Experimental resseting of the Campos Neto, M.C., 2000. Orogenic systems from southwestern U-Th-Pb systems in monazite. Chemical Geology, 191: Gondwana. An approach to Brasiliano-Pan African cycle and 165-181. collage in southeastern Brazil. In: Cordani, U.G, Milani, E.J., Thomaz Filho, A. and Campos D.A (Eds.), Tectonic Evolution Gibson, H. D., Carr, S. D., Brown, R. L. and Hamilton, M. A., 2004. of South America. Rio de Janeiro, 31st International Correlations between chemical and age domains in monazite, Geological Congress, 335-365. and metamorphic reactions involving major pelitic phases: an integration of ID TIMS and SHRIMP geochronology with Y and Campos Neto, M.C. and Caby, R., 1999. Neoproterozoic high- U X-ray mapping. Chemical Geology, 221: 237-260. pressure metamorphism and tectonic constraints from the nappe system south of the São Francisco Craton, southeast Hackspacher, P.C., Dantas, E.L., Spoladore, A., Fetter, A.H. and Brazil. Precambrian Research, 97: 3-26. Oliveira, M.A.F., 2000. Evidence for Neoproterozoic backarc basin development in the Central Ribeira Belt, Southeastern Campos Neto, M.C. and Figueiredo, M., 1995. The Rio Doce Brazil: new geochronological and geochemical constraints Orogeny, southeastern Brazil. Journal of South American from the São Roque - Açungui groups. Revista Brasileira de Earth Science, 8: 143-162. Geociências, 30: 110-114.

Cordani, U.G., Sato, K., Teixeira, W., Tassinari, C.C.G. and Hackspacher, P.C., Fetter, A.H., Ebert, H.D., Janasi, V.A., Basei, M.A.S., 2000. Crustal evolution of the South American Dantas, E.L., Oliveira, M.A.F. and Braga, I., 2003. Platform. In: Cordani, U.G, Milani, E.J., Thomaz Filho, A. and Magmatismo cálcio-alcalino há ca 660-640 Ma no Domínio Campos D.A (Eds.), Tectonic Evolution of South America. Rio Socorro: Registros de convergência pré-colisional na de Janeiro, 31st International Geological Congress, 19-40. aglutinação do Gondwana Ocidental. Geologia USP Série CPRM, 2002. Geologia e Recursos Minerais do Brasil. SIG 1:2 Científica, São Paulo 3; 85-96. 500 000. Hackspacher P.C. and Godoy A.M., 1999. Vertical displacement De Wit, M.J., Bowring, S, Ashwal, L.D., Randrianasolo, L.G., during late-collisional escape tectonics (Brasiliano Orogeny) Morel, V.P.I. and Rambeloson, R.A., 2001. Age and tectonic in the Ribeira belt, São Paulo State, Brazil. Journal of African evolution of Neoproterozoic ductile shear zones in southern Earth Sciences, 29: 25-32. Madagascar, with implications for Gondwana studies. Tectonics, 20: 1-45. Hackspacher, P.C., Ribeiro, L.F.B., Ribeiro, M.C.S., Fetter, A.H., Hadler Neto, J.C., Tello, C.E.S. and Dantas, E.L., 2004. Ebert, H.D., Chemale, Jr.F., Babinski, M., Artur, A.C. and Van Consolidation and break-up of the South American Platform Schmus, W.R., 1996. Tectonic setting and U/Pb zircon dating in southeastern Brazil: tectonothermal and denudation of the plutonic Socorro Complex in the Transpressive Rio histories. Gondwana Research, 7: 91-101. Paraíba do Sul Shear Belt, SE Brazil. Tectonics, 5: 688-699. Hasui, Y., Ebert, H.D. and Costa, J.B.S., 1990. Estruturação da Ebert, H.D. and Hasui, Y., 1998. Transpressional tectonics and extremidade oriental da chamada Cunha de Guaxupé. 36º strain partitioning during oblique collision between three Congresso Brasileiro de Geologia., SBG, Natal, Anais, 5: plates in the Precambrian of southeast Brazil. In: Holdsworth, 2296-2308. R.E., Strachan, R.A. and Dewey. J.F. (Eds.), Continental Transpressional/Transtensional Tectonics, Geological Heilbron, M. and Machado, N.M., 2003. Timing of terrane Society, London, Special Publications, 135: 231-252. accretion in the Neoproterozoic-Eopaleozoic Ribeira orogen (SE-Brazil). Precambrian Research, 125: 87-112. Ferreira Filho, C.F., Kamo, S., Fuck, R.A., Krogh, T.E. and Naldrett, A.J., 1994. Zircon and rutile geochronology of the Heilbron, M., Pedrosa-Soares, A.C., Campos Neto, M., Silva, Niquelândia layered mafic and ultramafic intrusion, Brazil: L.C., Trouw, R.A.J. and Janasi, V., 2004. Província constraints for the timing of magmatism and high grade Mantiqueira. In: Mantesso-Neto, V., Bartorelli, A., Carneiro, metamorphism. Precambrian Research, 68: 241-255. C.D.R. and Brito Neves, B.B. (Eds.), Geologia do Continente Sul-Americano: Evolução da Obra de Fernando Flávio Fischel, D.P., Pimentel, M.M. and Fuck, R.A., 1998. Idade de Marques de Almeida. Beca, São Paulo. 203-234 p. metamorfismo de alto grau no Complexo Anápolis-Itauçu, determinada pelo método Sm-Nd. Revista Brasileira de Janasi, V.A., Leite, R.J. and Van Schmus, W.R., 2001. U-Pb Geociências, 28: 543-544. chronostratigraphy of the granitic magmatism in the Agudos Grandes Batholith (west of São Paulo, Brazil) – implications Fleck, R.J., Sutter, J.F. and Elliot, D.H., 1977. Interpretation of for the evolution of the Ribeira belt. Journal of South American discordant 40Ar/39Ar age-spectra of Mesozoic tholeiites from Earth Sciences, 14: 363-376. Antarctica. Geochimica et Cosmochimica Acta, 41: 15-32

Foster, G., Parrish, R.R., Horstwood, M.S.A., Cherney, S, Pyle, J. and Gibson, H.D., 2004. The generation of prograde PTt points and paths: a textural, compositional, and chronological study of metamorphic monazites. Earth and Planetary Science Letters, 228: 125-142.

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 17 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Janasi, V.A., Vlach, S.R.F. and Ulbrich, H.H.G.J., 1993. Piuzana, D., Pimentel, M.M, Armstrong, R. and Fuck, R.A., 2002. Enriched-mantle contributions to the Itu granitoid belt, SHRIMP U-Pb and Sm-Nd geochronology of the Anápolis- southeastern Brazil: evidence from K-rich diorites and Itauçu Complex and associated granites: Neoproterozoic syenites. In: Sial, A.N. and Ferreira, V.P. (Eds.), Proceedings magmatism and high grade metamorphism in the Brasília belt, of the Workshop MAGMA. Anais da Academia Brasileira de Central Brazil. Precambrian Research, 125: 139-160. Ciências, 65:107-118. Renne, P.R., Swisher, C.C., Deino, A.L., Karner, D. B., Owens, Junges, S.L., Pimentel, M.M., and Moraes, R., 2002. Nd isotopic T.L. and DePaolo, D.J., 1998. Intercalibration of standards, study of the Neoproterozoic Mara Rosa Arc, central Brazil: absolute ages and uncertainties in 40Ar/39Ar dating. implications for the evolution of the Brasília Belt. Precambrian Chemical Geology, 145: 117-152. Research, 117; 101-118. Ribeiro, A., Trouw, R.A.J., Andreis, R.R., Paciullo, F.V.P. and Krogh, T.E., 1973. A low contamination method for hydrothermal Valença, J.G., 1995. Evolução das bacias Proterozóicas e o decomposition of zircon and extraction of U and Pb for isotopic termo-tectonismo Brasiliano na margem sul do Cráton de São age determinations. Geochimica et Cosmochimica Acta, 37: Francisco. Revista Brasileira de Geociências, 25: 235-248. 485-494. Stacey, J.S. and Kramers, J.D., 1975. Approximation of terrestrial Ludwig, K.R., 1999. ISOPLOT/EX (A plotting and regression lead isotope evolution by a two-stage model. Earth and program for radiogenic-isotope data) version 2.05. Berkley Planetary Science Letters, 26: 207-221. Geochronological Center, Special Publication 1A, 51 p. Steiger, R.H. and Jäger, E., 1977. Subcommission on Machado N., Valladares C.S., Heilbron M. and Valeriano C.M., Geochronology- convention and use of decay constants in 1996. U-Pb geochronology of the central Ribeira belt (Brazil) geochronology and cosmochronology. Earth and Planetary and implications for the evolution of the Brazilian Orogeny. Science Letters, 36: 359-362. Precambrian Research, 79: 347-361. Schmitt, R. S., Trouw, R.A.J. and Van Schmus, W.R., 1999. The McDougall, I. and Harrison, T.M., 1999. Geochronology and characterization of a Cambrian (520 Ma) tectonometamorphic Thermochronology by the 40Ar/39Ar method. 2nd ed., Oxford event in the coastal domain of the Ribeira belt (SE Brazil) University Press, 269p. using U/Pb in syntectonic veins. II South American Symposium on Isotope Geology (Córdoba, Argentina), Actas, Noce, C.M., Pedrosa-Soares, A.C., Piuzana, D., Armstrong, R., 363-366. Laux, J.H., Campos, C.M. and Medeiros, S.R., 2004. Ages of sedimentation of the kinzigitic complex and of a late orogenic Teixeira, A.L., Cordani, U.G. and Nutman, A., 1999. Idades U/Pb thermal episode in the Araçuaí Orogen, northern Espírito (SHRIMP) de seixo riolítico em metaconglomerado da Bacia Santo State, Brazil: zircon and monazite U-Pb shrimp and ID- Eleutério, Estado de São Paulo. Anais da Academia Brasileira TIMS data. Revista Brasileira de Geociências, 34: 587-592. de Ciências, 71: 837-838.

Paciullo, F.V.P., Ribeiro, A., Andreis, R.R. and Trouw, R.A.J., Töpfner, C., 1996. Brasiliano-Granitoide in den Bundesstaaten 2000. The Andrelândia Basin, a Neoproterozoic intraplate São Paulo und Minas Gerais, Brasilien – Eine Vergleichende continental margin, southern Brasília belt, Brazil. Revista Studie. Münchner Geologische Hefte, A17; 258p. Brasileira de Geociências, 30: 200-202. Trompette, R., 1994. Geology of Western Gondwana (2000-500 Pimentel, M.M., Ferreira Filho, C.M. and Armstrong, R.A., 2004a. Ma) Pan-African-Brasiliano Aggregation of South America SHRIMP U-Pb and Sm-Nd ages of the Niquelândia layered and Africa. Rotterdam, A.A. Balkema. 350 p. complex: Meso- (1.25 Ga) and Neoproterozoic (0.79 Ga) extensional events in central Brazil. Precambrian Research, Trouw, R.A.J., Heilbron, M., Ribeiro, A., Paciullo, F., Valeriano, 132: 133-153. C.M., Almeida, J.C.H., Tupinambá, M. and Andreis, R.R., 2000. The central segment of Ribeira belt. In: Cordani, U.G., Pimentel, M.M, Jost, H. and Fuck, R.A., 2004b. O embasamento Milani, E.J., Thomaz Filho, A. and Campos, D.A. (Eds.), da Faixa Brasília e o Arco Magmático de Goiás. In: Mantesso- Tectonic Evolution of South America. Rio de Janeiro, 31st Neto, V., Bartorelli, A., Carneiro, C.D.R. and Brito Neves, B.B. International Geological Congress, 287-310. (Eds.), Geologia do continente Sul-Americano: Evolução da Obra de Fernando Flávio Marques de Almeida. Beca, São Trouw, R.A.J. and Pankhurst, R.J., 1993. Idades radiométricas Paulo. 355-368. ao sul do Cráton do São Francisco: região da Folha Barbacena, Minas Gerais. In: II Simposio do Cráton do São Pimentel, M.M, Fuck, R.A., Jost, H., Ferreira Filho, C.F. and Francisco, Salvador, BA, Anais, 260-262. Araújo, S. M., 2000. The basement of the Brasília Fold Belt and the Goiás Magmatic Arc. In: Cordani, U.G., Milani, E.J., Tupinambá, M., Teixeira, W. and Heilbron, M., 2000. Thomaz Filho, A. and Campos, D.A. (Eds.): Tectonic Neoproterozoic western Gondwan assembly and subduction- Evolution of South America. Rio de Janeiro, 31st International related plutonism: the role of the Rio Negro Complex in the Geological Congress, 195-230. Ribeira Belt, southeastern Brazil. Revista Brasileira de Geociências, 30: 7-11.

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 18 Belt Tectonics Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Valeriano, C.M., Dardenne, M.A., Fonseca, M.A., Simões, L.S.A. A. 40Ar/39Ar analytical data and Seer, H.J., 2004. A evolução tectônica da Faixa Brasília. In: Mantesso-Neto, V., Bartorelli, A., Carneiro, C.D.R. and Table A.1. 40Ar/39Ar analytical data (single grains; Brito Neves, B.B. (Eds), Geologia do Continente Sul- triplicate) from the southern Brasília belt Americano: Evolução da Obra de Fernando Flávio Marques de Almeida. Beca, São Paulo, pp. 575-592. Sa M La La 40/ 38/ 37/ 36/ 40 Ar % Ag ± Vasconcelos, P. M., Onoe, A. T., Kawashita, K., Soares, A. J. and m ate b# ser 39 39 39 39 */ 40 Ra e Teixeira, W., 2002. 40Ar/39Ar geochronology at the Instituto ple ria 39 d de Geociências, USP: instrumentation, analytical procedures, and calibration. Anais da Academia Brasileira de Ciências, l 74; 297-342. ( ( ( ( Wernick, W., 1998. The pluriserial Ribeira magmatic system, SE/ W) mo M M S Brazil and Uruguay. Revista Brasileira de Geociências, 28: ls) a) a) 533-542. SP Wiedemann, C., 1993. The evolution of the early Paleozoic, late A0 to post-collisional magmatic arc of the coastal mobile belt, in the state of Espírito Santo, eastern Brazil. Anais da Academia 10 Brasileira de Ciências, 65: 162-181. 4-4 6 Zanardo, A. and Oliveira, M.A.F., 1990. Aspectos microestruturais e texturais dos metassedimentos da DI mu 09 0.2 34. 0.0 0.0 0.0 18. 3.7 54. 52 99. Formação Eleutério. Geociências, (special volume): 317-330. T sco 18- 0 99 37 00 54 98 3E 3 8.3 59 vit 01 55 62 00 17 69 -16 8 e A 4 1 09 0.3 22. 0.0 0.1 0.0 2.6 3.5 12. 83. 78. 18- 5 02 67 35 65 35 7E 0 27 50 01 48 64 30 65 82 -16 B 3 09 0.5 21. 0.0 0.0 0.0 20. 6.7 96. 56 27. 18- 0 07 11 00 02 33 5E 5 0.5 11 01 18 66 00 50 11 -16 2 C 4 0 09 0.7 19. 0.0 0.0 0.0 17. 2.2 89. 48 9.8 18- 0 36 16 00 06 36 8E 7 8.7 0 01 44 06 00 77 38 -15 9 D 1 6 09 0.9 20. 0.0 0.0 0.0 18. 7.7 87. 50 3.9 18- 0 62 13 00 08 02 2E 4 5.1 0 01 36 91 00 78 88 -15 2 E 6 9 09 1.2 18. 0.0 0.0 0.0 17. 5.4 98. 49 3.2 18- 0 13 09 00 01 76 3E 0 8.7 8 01 21 25 00 23 86 -14 5 F 1 9 09 1.5 17. 0.0 0.0 0.0 17. 1.7 99. 49 1.4 18- 0 88 10 00 00 77 5E 4 9.0 8 01 91 15 00 37 88 -13 0 G 7 6 09 1.8 17. 0.0 0.0 0.0 17. 8.5 99. 49 2.7 18- 0 58 11 00 00 57 1E 9 4.0 0 40 39 Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and Ar/ Ar evidence for overprinting01 88 of the07 Brasília00 Belt04 by57 the Ribeira-14 1 Page 19 Belt Tectonics H 0 0 09 2.2 17. 0.0 0.0 0.0 17. 1.2 98. 48 3.4 18- 1 35 10 03 00 17 1E 9 4.1 2 01I 95 00 48 63 41 -14 1 4 0 09 2.6 17. 0.0 0.0 -0. 17. 7.1 10 49 3.8 18- 0 49 10 04 00 80 6E 1.8 9.6 0 01 72 05 84 10 39 -15 1 J 2 4 6 09 3.0 17. 0.0 0.0 0.0 17. 4.6 99. 50 5.3 18- 0 89 09 00 00 85 3E 8 0.8 0 01 62 53 00 15 26 -15 1 K 8 4 09 3.5 17. 0.0 0.0 0.0 17. 1.0 98. 49 3.4 18- 0 71 11 00 00 47 4E 7 1.5 5 01 01 07 00 79 60 -14 6 L 3 6 09 4.0 17. 0.0 0.0 -0. 18. 6.5 10 50 6.4 18- 1 56 08 00 00 06 5E 2.8 5.9 2 01 51 43 00 16 22 -15 3 M 6 8 2 09 5.0 17. 0.0 0.0 0.0 17. 2.9 99. 49 6.9 18- 0 71 10 00 00 62 7E 5 5.1 1 01 97 36 98 32 36 -14 9 N 9 5 09 0.4 31. 0.0 0.0 0.0 17. 4.0 55. 48 76. 18- 0 01 40 00 46 22 7E 5 5.3 90 02 90 78 00 69 23 -16 0 A 4 0 09 0.7 19. 0.0 0.0 0.0 15. 9.6 77. 43 21. 18- 0 74 17 22 14 38 7E 9 9.2 47 02 24 66 85 76 22 -16 6 B 1 5 09 1.0 23. 0.0 0.0 0.0 15. 6.8 68. 45 10. 18- 0 14 15 00 24 86 4E 6 1.5 42 02 36 51 00 61 98 -15 7 C 9 0 09 1.3 18. 0.0 0.0 0.0 17. 8.2 98. 50 5.6 18- 0 11 10 00 00 89 5E 8 1.9 6 02 69 38 00 73 97 -14 6 D 1 4 09 1.3 17. 0.0 0.0 0.0 17. 8.6 99. 49 1.7 18- 0 69 11 00 00 63 8E 7 5.4 7 02 01 42 00 19 21 -14 0 E 8 3 09 1.5 17. 0.0 0.0 0.0 17. 4.2 98. 49 1.3 18- 0 74 11 00 01 43 3E 3 0.5 2 02 16 11 00 04 36 -14 2 F 1 6 09 1.8 17. 0.0 0.0 0.0 17. 1.1 99. 49 1.1 18- 0 66 10 00 00 61 7E 7 5.0 5 02 63 87 51 16 73 -13 3 G 2 5 09 2.4 17. 0.0 0.0 0.0 17. 7.4 98. 48 3.1 18- 0 45 11 00 00 20 9E 5 4.8 1 02 74 70 17 86 33 -15 3 H 0 3 09 3.5 17. 0.0 0.0 -0. 17. 9.3 10 49 3.4 18- 0 52 10 04 00 72 9E 1.1 7.6 1 02I 78 52 18 06 55 -15 9 0 7 2 09 4.2 17. 0.0 0.0 -0. 17. 1.1 10 50 2.4 18- 1 68 09 00 00 83 9E 0.8 0.4 7 02 86 26 00 05 77 -14 4 J 7 1 6 09 5.0 17. 0.0 0.0 0.0 17. 4.1 10 50 1.2 18- 0 90 10 00 00 89 8E 0.0 1.9 2 02 38 49 00 01 96 -14 6 K 3 4 09 0.4 28. 0.0 0.0 -0. 33. 2.3 11 85 85. 18- 0 69 25 00 01 69 6E 7.4 2.3 68 03 80 84 00 69 76 -16 5 A 0 2 3 09 0.7 19. 0.0 0.0 -0. 19. 4.7 10 54 34. 18- 0 08 11 00 00 79 0E 3.7 7.8 96 03 91 42 00 24 72 -16 2 B 4 0 7 09 1.0 18. 0.0 0.0 -0. 19. 1.9 10 53 10. 18- 0 75 08 00 00 17 0E 2.3 3.0 75 03 24 16 00 14 98 -15 3 C 8 5 0 09 1.3 18. 0.0 0.0 0.0 17. 2.7 97. 50 5.0 18- 0 39 09 00 01 91 4E 4 2.3 0 03 15 75 00 61 52 -14 4 D 5 5 09 1.5 17. 0.0 0.0 0.0 17. 1.9 99. 49 1.0 18- 0 82 10 00 00 80 3E 8 9.5 2 03 79 49 90 09 05 -13 3 E 5 1 09 1.8 17. 0.0 0.0 0.0 17. 1.4 99. 48 2.7 18- 0 44 10 60 00 26 2E 0 6.4 6 03 43 43 87 61 99 -14 8 F 2 4 09 2.3 17. 0.0 0.0 -0. 17. 7.3 10 50 2.7 18- 9 71 11 25 00 88 8E 1.0 1.7 5 03 74 39 68 05 94 -15 1 G 0 8 6 09 3.0 17. 0.0 0.0 -0. 18. 1.5 10 52 11. 18- 0 96 04 41 00 80 8E 4.6 3.8 37 03 87 54 15 28 01 -15 7 H 0 0 0 09 4.0 17. 0.0 0.0 -0. 18. 1.0 10 50 2.4 18- 1 98 10 00 00 00 6E 0.1 4.5 0 03I 77 66 00 00 45 -14 2 3 6 5 09 5.0 17. 0.0 0.0 -0. 17. 2.5 10 50 1.1 18- 0 83 10 00 00 90 4E 0.4 2.0 2 03 57 35 00 02 45 -14 8 J 6 4 0 DI bi- 09 0.2 9.0 0.0 0.1 0.0 3.3 3.3 37. 10 33. T otit 19- 0 68 11 29 19 75 7E 2 5.9 18 e 01 44 52 38 30 37 -16 6 A 09 0.3 17. 0.0 0.0 -0. 17. 3.6 10 50 5.6 19- 2 50 10 00 00 91 1E 2.3 2.3 2 01 87 24 00 13 60 -15 6 B 0 8 5 09 0.5 17. 0.0 0.0 0.0 17. 2.2 98. 48 1.7 19- 0 40 12 03 00 15 8E 6 3.7 7 01 20 62 12 82 83 -14 2 C 7 7 09 0.7 17. 0.0 0.0 0.0 17. 3.5 99. 48 2.8 19- 0 47 10 01 00 37 5E 5 9.1 3 01 02 79 49 31 71 -14 2 D 0 4 09 0.9 17. 0.0 0.0 0.0 17. 3.2 99. 48 2.0 19- 0 43 10 00 00 40 0E 8 9.7 4 01 01 52 56 09 24 -14 5 E 0 5 09 1.1 17. 0.0 0.0 -0. 17. 3.5 10 49 3.3 19- 0 50 09 00 00 52 6E 0.1 2.8 4 01 69 84 43 00 69 -14 1 F 3 7 6 09 1.4 17. 0.0 0.0 -0. 17. 6.4 10 49 0.9 19- 0 60 10 00 00 65 3E 0.3 5.9 5 01 19 90 50 01 51 -14 6 G 4 8 4 09 1.7 17. 0.0 0.0 -0. 17. 4.0 10 49 1.0 19- 0 70 10 00 00 81 0E 0.6 9.8 5 01 68 84 00 03 38 -14 6 H 6 6 6 09 2.0 17. 0.0 0.0 -0. 17. 2.5 10 49 1.1 19- 1 62 10 00 00 72 7E 0.6 7.6 4 01I 44 76 00 03 46 -14 7 7 4 1 09 2.3 17. 0.0 0.0 -0. 17. 1.8 10 49 2.6 19- 1 36 09 00 00 53 0E 1.0 3.0 6 01 75 27 00 05 67 -14 5 J 3 8 5 09 2.8 17. 0.0 0.0 -0. 17. 1.7 10 49 2.3 19- 0 52 10 00 00 58 8E 0.3 4.1 2 01 12 27 00 02 15 -14 5 K 9 1 2 09 3.5 17. 0.0 0.0 0.0 17. 3.9 99. 49 5.3 19- 0 67 12 00 00 60 2E 6 4.8 7 01 41 52 00 22 98 -15 5 L 7 6 09 4.2 17. 0.0 0.0 -0. 19. 8.5 11 54 19. 19- 1 13 08 15 00 79 0E 5.5 7.6 60 01 69 44 69 89 08 -16 7 M 3 8 8 09 5.0 17. 0.0 0.0 -0. 17. 9.5 10 49 3.0 19- 0 55 10 00 00 59 5E 0.3 4.5 2 01 17 49 00 01 92 -15 9 N 3 6 0 09 0.3 17. 0.0 0.0 0.0 15. 3.5 87. 43 5.1 19- 0 44 12 03 07 23 8E 3 5.5 9 02 96 26 72 48 77 -15 9 A 0 8 09 0.5 17. 0.0 0.0 0.0 17. 2.2 98. 48 2.2 19- 0 62 10 00 01 29 2E 1 7.0 6 02 77 16 00 13 43 -14 8 B 1 6 09 0.7 17. 0.0 0.0 0.0 17. 2.5 99. 49 1.7 19- 0 73 11 00 00 55 2E 0 3.5 8 02 41 86 14 60 57 -14 2 C 6 6 09 1.0 17. 0.0 0.0 0.0 17. 4.4 99. 49 1.6 19- 0 76 10 00 00 75 7E 9 8.3 4 02 37 74 00 03 34 -14 8 D 6 8 09 1.3 17. 0.0 0.0 0.0 17. 6.6 99. 49 0.8 19- 0 72 10 00 00 68 9E 8 6.7 7 02 86 86 89 13 82 -14 8 E 8 4 09 1.6 17. 0.0 0.0 -0. 17. 4.0 10 49 1.5 19- 0 64 09 00 00 69 0E 0.3 6.9 7 02 86 89 00 01 51 -14 5 F 9 6 6 09 2.0 17. 0.0 0.0 -0. 17. 2.0 10 49 1.9 19- 1 72 10 00 00 74 4E 0.1 8.2 7 02 87 63 00 00 81 -14 5 G 3 7 5 09 2.5 17. 0.0 0.0 -0. 18. 2.0 10 51 11. 19- 0 78 13 00 00 60 3E 4.6 9.0 14 02 85 22 00 27 00 -15 2 H 2 5 0 09 3.0 17. 0.0 0.0 0.0 17. 9.4 98. 48 17. 19- 1 44 02 00 00 20 7E 6 4.8 78 02I 78 17 00 83 27 -16 2 3 7 09 3.5 17. 0.0 0.0 -0. 19. 7.1 11 54 22. 19- 0 62 12 00 00 49 2E 0.6 0.5 45 02 88 27 00 63 10 -16 0 J 7 0 4 09 4.2 17. 0.0 0.0 0.0 9.3 6.6 54. 28 24. 19- 1 40 35 97 27 99 4E 0 0.8 52 02 58 33 33 12 86 -16 8 K 6 09 5.0 18. 0.0 0.0 0.0 17. 8.0 96. 49 3.6 19- 0 06 12 00 01 49 5E 8 2.1 5 02 92 56 00 93 83 -15 1 L 9 6 DI bi- 09 0.3 16. 0.0 0.0 0.0 15. 1.5 98. 45 10. T otit 19- 0 12 06 00 01 81 5E 1 0.0 98 e 03 10 72 00 05 03 -15 7 A 8 6 09 0.5 17. 0.0 0.0 0.0 16. 2.2 98. 47 1.9 19- 0 26 11 01 00 98 7E 4 9.5 0 03 61 04 30 94 85 -14 2 B 1 5 09 0.9 17. 0.0 0.0 0.0 17. 7.5 99. 48 1.0 19- 0 46 10 00 00 38 7E 6 9.3 1 03 21 91 00 26 56 -14 3 C 3 2 09 1.2 17. 0.0 0.0 -0. 17. 7.0 10 48 1.8 19- 0 34 11 00 00 35 2E 0.0 8.5 3 03 91 23 00 00 38 -14 5 D 8 2 8 09 1.4 17. 0.0 0.0 0.0 17. 5.7 10 49 0.9 19- 0 52 11 00 00 51 6E 0.0 2.5 7 03 36 33 36 02 66 -14 6 E 2 3 09 1.8 17. 0.0 0.0 0.0 17. 6.8 99. 49 3.3 19- 0 60 10 00 00 59 1E 9 4.4 5 03 36 65 00 03 28 -14 3 F 7 5 09 2.5 17. 0.0 0.0 0.0 17. 5.7 99. 49 0.9 19- 0 59 11 01 00 56 3E 8 3.7 0 03 91 47 35 12 40 -14 2 G 0 0 09 3.0 17. 0.0 0.0 0.0 16. 5.8 98. 47 4.1 19- 0 30 11 17 01 95 8E 0 8.8 5 03 60 03 16 17 98 -15 0 H 7 4 09 4.2 17. 0.0 0.0 0.0 17. 3.9 98. 48 5.3 19- 1 47 13 15 01 17 0E 3 4.2 2 03I 79 87 19 02 80 -15 1 4 7 09 5.0 17. 0.0 0.0 0.0 17. 1.7 99. 49 1.9 19- 0 56 11 33 00 53 9E 8 3.0 2 03 50 22 65 11 58 -14 3 J 9 9 A mu 09 0.2 19. 0.0 0.0 0.0 18. 4.2 96. 52 45. N sco 21- 0 37 11 00 02 73 2E 7 2.4 05 DT vit 01 17 36 00 14 97 -16 1 e A 9 6 09 0.3 18. 0.0 0.0 0.0 18. 1.1 96. 50 17. 21- 5 71 00 28 01 13 3E 9 7.7 60 01 90 23 98 97 82 -15 9 B 8 4 09 0.5 22. 0.0 0.0 0.0 16. 3.0 76. 47 9.3 21- 0 17 13 03 17 96 0E 5 8.8 6 01 86 88 08 65 13 -15 4 C 0 4 09 0.7 18. 0.0 0.0 0.0 17. 2.4 96. 49 3.9 21- 0 19 10 00 02 56 0E 6 3.8 0 01 53 33 00 12 91 -14 5 D 0 9 09 0.9 17. 0.0 0.0 0.0 17. 9.1 99. 49 1.6 21- 0 85 11 00 00 78 1E 6 9.1 2 01 18 36 00 23 38 -14 2 E 7 7 09 1.2 17. 0.0 0.0 0.0 17. 1.5 99. 50 0.9 21- 0 85 10 01 00 82 4E 8 0.2 7 01 64 62 89 09 78 -13 0 F 3 9 09 1.5 17. 0.0 0.0 0.0 17. 7.9 99. 49 1.3 21- 0 72 10 00 00 69 2E 9 6.9 8 01 12 42 00 09 45 -14 3 G 0 3 09 1.8 17. 0.0 0.0 -0. 17. 2.8 10 50 1.2 21- 0 80 10 00 00 84 0E 0.2 0.6 9 01 84 35 00 01 76 -14 9 H 4 4 8 09 2.2 17. 0.0 0.0 -0. 18. 1.6 10 50 2.2 21- 1 97 10 00 00 05 2E 0.5 5.7 2 01I 48 14 00 02 57 -14 8 9 8 3 09 2.6 17. 0.0 0.0 -0. 17. 1.2 10 49 2.5 21- 0 74 09 00 00 80 4E 0.3 9.5 1 01 77 50 00 01 27 -14 8 J 1 9 3 09 3.0 17. 0.0 0.0 0.0 17. 1.3 98. 49 3.3 21- 1 81 12 01 00 60 7E 8 4.7 5 01 62 77 71 71 50 -14 3 K 6 2 09 3.6 17. 0.0 0.0 0.0 17. 2.5 10 50 2.0 21- 1 84 10 00 00 83 5E 0.0 0.4 2 01 46 48 00 02 74 -14 4 L 1 5 09 4.2 17. 0.0 0.0 0.0 17. 1.3 98. 48 3.8 21- 1 49 10 00 00 26 4E 7 6.3 3 01 55 29 00 78 32 -14 1 M 4 1 09 5.0 17. 0.0 0.0 0.0 17. 2.3 99. 49 1.3 21- 0 89 11 00 00 80 9E 5 9.7 4 01 14 57 00 28 92 -14 4 N 0 3 09 0.4 17. 0.0 0.1 0.0 10. 4.1 56. 29 44. 21- 0 70 17 19 25 05 9E 8 8.8 91 02 76 98 41 94 31 -16 7 A 5 7 09 0.7 19. 0.0 0.0 0.0 16. 2.3 88. 47 8.9 21- 0 21 17 18 07 99 0E 4 9.6 8 02 50 03 60 52 24 -15 1 B 2 6 09 0.9 18. 0.0 0.0 0.0 17. 1.3 97. 49 2.3 21- 0 35 11 03 01 81 7E 1 9.8 8 02 33 68 37 82 48 -14 8 C 3 0 09 1.1 18. 0.0 0.0 0.0 17. 6.0 99. 50 1.4 21- 1 01 10 00 00 99 1E 9 4.2 7 02 44 96 24 07 35 -14 6 D 7 3 09 1.3 18. 0.0 0.0 0.0 18. 9.4 99. 50 1.4 21- 0 06 11 00 00 01 6E 7 4.7 1 02 15 01 65 17 19 -14 1 E 5 7 09 1.5 18. 0.0 0.0 0.0 17. 3.5 99. 50 1.9 21- 0 07 11 00 00 94 7E 3 3.0 3 02 32 56 27 43 41 -14 5 F 8 9 09 1.9 18. 0.0 0.0 -0. 18. 1.1 10 52 15. 21- 0 53 10 00 00 81 3E 1.5 4.2 30 02 66 59 00 09 49 -14 3 G 2 4 3 09 2.6 17. 0.0 0.0 0.0 17. 9.0 98. 48 2.5 21- 0 63 11 01 01 27 1E 0 6.5 6 02 45 00 20 22 37 -15 7 H 0 6 09 3.6 18. 0.0 0.0 0.0 18. 2.3 99. 50 2.7 21- 1 18 10 00 00 10 8E 6 7.1 3 02I 20 54 00 24 98 -14 0 3 1 09 5.0 17. 0.0 0.0 0.0 17. 3.3 99. 50 1.0 21- 1 98 11 01 00 86 3E 4 1.2 8 02 39 77 63 39 92 -14 1 J 6 4 09 0.4 19. 0.0 0.0 0.0 14. 1.8 75. 42 11. 21- 0 77 20 10 16 89 9E 3 6.7 97 03 37 79 07 53 02 -15 4 A 0 1 09 0.7 17. 0.0 0.0 0.0 17. 6.7 99. 50 1.0 21- 0 93 11 00 00 87 4E 6 1.2 0 03 93 17 62 23 05 -14 5 B 7 4 09 0.9 18. 0.0 0.0 0.0 17. 4.6 98. 50 0.9 21- 0 07 10 00 00 86 8E 8 1.0 8 03 46 90 00 72 15 -14 3 C 4 6 09 1.1 18. 0.0 0.0 0.0 18. 1.0 98. 51 2.2 21- 0 81 10 00 00 58 8E 7 8.5 0 03 76 15 00 80 00 -14 4 D 2 7 09 1.3 18. 0.0 0.0 0.0 17. 1.2 96. 49 2.8 21- 0 23 12 00 01 65 8E 8 5.8 6 03 98 87 00 99 11 -14 6 E 8 4 09 1.5 17. 0.0 0.0 0.0 17. 2.6 99. 49 1.6 21- 0 87 10 00 00 80 9E 6 9.6 4 03 49 87 00 23 67 -14 8 F 5 3 09 1.9 17. 0.0 0.0 0.0 17. 7.0 99. 50 1.7 21- 0 84 11 00 00 82 3E 9 0.0 6 03 42 29 00 07 18 -14 5 G 8 9 09 2.4 17. 0.0 0.0 0.0 17. 2.0 99. 49 1.7 21- 0 84 10 00 00 81 8E 8 9.8 0 03 35 62 00 11 16 -14 0 H 9 4 09 3.0 17. 0.0 0.0 0.0 17. 1.9 99. 50 1.7 21- 1 95 09 00 00 92 2E 8 2.6 0 03I 98 89 00 11 68 -14 2 7 2 09 3.6 17. 0.0 0.0 0.0 16. 5.9 95. 47 4.2 21- 1 75 11 00 02 97 6E 6 9.2 5 03 54 15 00 63 66 -15 2 J 9 6 09 4.2 17. 0.0 0.0 -0. 18. 3.9 10 51 5.0 21- 2 90 07 00 00 35 0E 2.6 3.1 7 03 06 45 00 15 69 -15 2 K 0 5 7 09 5.0 18. 0.0 0.0 0.0 17. 1.9 98. 50 1.5 21- 0 04 11 00 00 84 5E 9 0.7 1 03 34 20 00 66 83 -14 0 L 4 0 LU mu 09 0.2 22. 0.0 0.0 0.0 14. 6.0 63. 41 35. M sco 22- 0 62 08 00 28 30 2E 2 1.6 39 E vit 01 65 81 00 17 01 -16 2 e A 0 6 09 0.3 19. 0.0 0.0 0.0 16. 2.4 87. 47 8.3 22- 5 07 13 30 08 61 2E 1 0.2 2 01 25 04 12 33 35 -15 0 B 2 6 09 0.5 18. 0.0 0.0 -0. 18. 8.1 10 52 2.7 22- 0 62 10 00 00 80 3E 1.0 3.8 0 01 38 42 00 06 10 -15 9 C 5 0 7 09 0.7 19. 0.0 0.0 0.0 19. 4.6 99. 53 2.0 22- 0 38 10 00 00 23 8E 2 4.4 8 01 74 77 54 50 80 -14 3 D 4 9 09 0.9 19. 0.0 0.0 0.0 19. 1.3 99. 52 1.5 22- 0 05 11 00 00 00 3E 7 8.8 0 01 81 54 14 18 46 -13 1 E 3 1 09 1.2 19. 0.0 0.0 0.0 19. 1.5 99. 53 3.1 22- 0 16 10 00 00 09 3E 6 0.8 2 01 22 17 00 24 06 -13 8 F 0 4 09 1.5 18. 0.0 0.0 0.0 18. 7.3 99. 51 1.8 22- 0 45 10 00 00 40 7E 7 4.1 4 01 29 36 00 18 04 -14 8 G 8 2 09 1.8 18. 0.0 0.0 0.0 18. 3.2 99. 51 1.2 22- 0 62 10 00 00 52 2E 4 7.1 4 01 75 78 00 36 16 -14 2 H 2 3 09 2.2 19. 0.0 0.0 0.0 19. 2.8 99. 53 1.1 22- 1 10 11 00 00 08 5E 9 0.8 4 01I 15 00 00 04 94 -14 5 9 3 09 2.6 18. 0.0 0.0 -0. 18. 9.1 10 52 4.6 22- 0 67 09 00 00 81 7E 0.7 4.1 0 01 32 43 00 04 07 -15 2 J 9 7 3 09 3.0 19. 0.0 0.0 0.0 18. 7.3 97. 52 4.1 22- 1 07 12 13 01 67 1E 9 0.8 6 01 07 58 88 34 50 -15 4 K 8 9 09 3.5 19. 0.0 0.0 0.0 18. 5.7 97. 52 4.1 22- 0 13 10 00 01 74 7E 9 2.5 2 01 90 55 00 33 41 -15 1 L 4 0 09 4.2 19. 0.0 0.0 0.0 18. 4.8 95. 50 4.8 22- 1 15 10 00 03 22 6E 2 9.9 3 01 31 88 10 13 85 -15 9 M 3 2 09 5.0 19. 0.0 0.0 0.0 19. 8.3 99. 53 3.1 22- 0 43 10 00 00 39 6E 8 8.1 6 01 56 26 00 15 13 -14 1 N 7 6 LU mu 09 0.3 20. 0.0 0.0 -0. 21. 3.1 10 58 7.3 M sco 22- 5 80 07 00 00 26 3E 2.2 2.4 0 E vit 02 40 60 00 15 19 -15 4 e A 1 5 6 09 0.5 18. 0.0 0.0 0.0 18. 7.9 98. 51 3.9 22- 0 68 10 00 01 36 3E 3 3.2 5 02 90 73 00 10 40 -15 9 B 0 7 09 0.7 19. 0.0 0.0 0.0 19. 8.0 99. 54 1.0 22- 0 69 10 00 00 59 9E 5 2.9 7 02 01 98 00 33 29 -14 4 C 5 6 09 0.9 19. 0.0 0.0 0.0 19. 1.2 99. 53 1.3 22- 0 26 11 00 00 21 3E 8 3.9 0 02 43 20 85 15 98 -13 9 D 3 0 09 1.1 18. 0.0 0.0 0.0 18. 8.5 99. 52 1.1 22- 1 94 11 00 00 93 7E 9 7.0 1 02 26 01 00 04 08 -14 3 E 4 9 09 1.6 18. 0.0 0.0 0.0 18. 1.0 99. 52 1.3 22- 0 86 10 00 00 83 2E 9 4.6 5 02 18 68 00 09 30 -13 6 F 0 6 09 2.5 18. 0.0 0.0 0.0 18. 1.7 99. 52 2.3 22- 0 96 10 00 00 93 4E 8 7.0 0 02 24 81 00 10 10 -14 3 G 9 8 09 3.4 19. 0.0 0.0 -0. 19. 1.0 10 53 2.8 22- 1 00 09 00 00 20 0E 1.0 3.6 9 02 79 44 00 06 43 -14 2 H 7 7 6 09 4.2 19. 0.0 0.0 -0. 19. 6.8 10 54 3.4 22- 1 24 09 00 00 65 9E 2.2 4.5 6 02I 30 64 00 14 93 -15 3 5 1 6 09 5.0 19. 0.0 0.0 -0. 19. 7.2 10 54 1.1 22- 0 51 10 00 00 53 4E 0.1 1.5 3 02 54 69 00 00 25 -14 0 J 7 6 9 09 0.3 19. 0.0 0.0 0.0 19. 2.4 96. 53 9.4 22- 5 95 06 00 02 14 2E 0 2.2 3 03 25 99 00 73 56 -15 1 A 0 8 09 0.5 18. 0.0 0.0 0.0 17. 4.7 98. 50 4.7 22- 0 20 10 00 01 86 7E 1 1.1 8 03 61 23 00 15 54 -15 2 B 1 8 09 0.7 19. 0.0 0.0 0.0 19. 5.5 99. 53 3.2 22- 0 20 10 00 00 10 2E 5 1.3 2 03 95 48 00 33 98 -14 4 C 6 9 09 0.9 18. 0.0 0.0 0.0 18. 9.1 99. 52 1.2 22- 0 70 10 00 00 66 7E 8 0.6 0 03 61 83 00 13 76 -14 6 D 0 2 09 1.2 18. 0.0 0.0 0.0 18. 1.0 99. 51 1.7 22- 0 45 10 00 00 42 8E 8 4.8 0 03 49 99 29 10 59 -13 0 E 6 5 09 1.5 18. 0.0 0.0 0.0 18. 3.6 99. 50 1.1 22- 0 26 10 00 00 19 8E 6 9.2 4 03 81 81 00 23 81 -14 5 F 4 0 09 2.0 18. 0.0 0.0 0.0 18. 1.1 99. 51 2.7 22- 1 35 10 00 00 23 7E 4 0.2 6 03 68 79 00 40 90 -14 5 G 5 3 09 2.9 18. 0.0 0.0 0.0 17. 6.9 96. 49 4.8 22- 0 20 11 00 02 61 4E 7 4.8 3 03 90 21 00 02 10 -15 8 H 6 0 09 4.0 18. 0.0 0.0 0.0 18. 4.7 96. 50 4.9 22- 1 90 10 00 02 17 4E 1 8.7 1 03I 57 69 00 47 60 -15 1 2 6 09 5.0 19. 0.0 0.0 0.0 18. 5.4 99. 52 1.1 22- 0 01 11 00 00 99 1E 9 8.6 6 03 01 01 00 04 85 -14 6 J 4 1 IT mu 09 0.2 15. 0.0 0.0 0.0 14. 1.0 95. 41 13. M sco 24- 0 21 09 00 02 52 5E 5 7.4 44 TR vit 01 74 09 15 34 60 -15 2 e A 0 7 09 0.3 17. 0.0 0.0 -0. 17. 3.5 10 49 5.3 24- 2 35 09 00 00 58 0E 1.3 4.2 1 01 64 57 00 07 51 -15 4 B 4 8 9 09 0.5 18. 0.0 0.0 0.0 18. 1.3 99. 51 1.7 24- 0 30 10 00 00 24 2E 7 0.4 7 01 06 54 00 18 53 -14 0 C 1 8 09 0.7 18. 0.0 0.0 0.0 18. 3.5 99. 50 1.0 24- 0 07 11 00 00 04 9E 8 5.4 5 01 56 41 00 11 10 -14 2 D 3 7 09 0.9 17. 0.0 0.0 -0. 17. 6.9 10 49 1.1 24- 0 80 09 00 00 81 3E 0.1 9.9 2 01 64 93 00 00 81 -14 6 E 7 4 6 09 1.1 17. 0.0 0.0 -0. 17. 3.7 10 49 0.9 24- 0 68 11 00 00 79 3E 0.6 9.3 2 01 44 05 00 03 32 -14 5 F 7 7 0 09 1.3 17. 0.0 0.0 -0. 18. 1.3 10 50 3.1 24- 0 66 10 00 00 08 5E 2.4 6.4 4 01 31 13 00 14 35 -14 5 G 8 2 1 09 1.6 17. 0.0 0.0 -0. 17. 9.6 10 49 2.3 24- 0 64 09 00 00 77 4E 0.7 8.8 4 01 25 49 00 04 23 -15 4 H 4 4 1 09 1.9 17. 0.0 0.0 0.0 17. 8.8 96. 48 2.6 24- 0 73 11 10 02 05 2E 2 1.2 6 01I 23 47 32 28 82 -15 4 9 5 09 2.4 17. 0.0 0.0 0.0 17. 1.3 99. 49 2.9 24- 0 69 10 01 00 63 9E 6 5.4 5 01 70 21 53 21 41 -14 5 J 1 6 09 3.0 17. 0.0 0.0 0.0 17. 1.5 99. 49 2.5 24- 0 83 10 00 00 70 8E 3 7.2 4 01 66 99 00 44 58 -14 1 K 3 8 09 3.6 17. 0.0 0.0 0.0 17. 1.1 99. 49 3.3 24- 1 66 11 03 00 61 4E 7 4.9 3 01 06 05 64 16 42 -14 6 L 3 7 09 4.2 18. 0.0 0.0 0.0 17. 6.5 98. 49 3.6 24- 1 04 09 00 00 78 9E 6 9.0 4 01 27 84 00 88 26 -15 9 M 1 8 09 5.0 18. 0.0 0.0 0.0 18. 9.7 98. 50 4.2 24- 1 50 10 00 01 17 0E 2 8.6 4 01 87 90 00 13 45 -15 8 N 4 6 09 0.2 10. 0.0 0.0 0.0 8.7 5.1 87. 26 23. 24- 0 01 21 00 04 91 8E 8 3.9 62 02 37 11 00 13 55 -16 7 A 0 09 0.3 16. 0.0 0.0 0.0 15. 2.5 95. 44 7.0 24- 5 52 10 00 02 73 0E 2 8.1 6 02 07 75 00 66 29 -15 2 B 2 3 09 0.6 17. 0.0 0.0 0.0 17. 1.3 99. 49 2.3 24- 0 84 11 00 00 72 5E 4 7.8 1 02 42 60 00 38 97 -14 0 C 5 8 09 0.8 18. 0.0 0.0 -0. 18. 2.0 10 50 1.4 24- 0 03 11 00 00 07 3E 0.2 6.1 3 02 44 09 00 01 00 -14 2 D 3 2 1 09 1.0 18. 0.0 0.0 -0. 18. 3.5 10 51 1.6 24- 0 23 09 00 00 36 8E 0.7 3.3 2 02 73 26 00 04 78 -14 8 E 1 4 7 09 1.2 18. 0.0 0.0 0.0 18. 6.8 10 50 0.9 24- 0 07 11 00 00 06 5E 0.0 6.0 0 02 35 11 00 02 81 -14 8 F 5 7 09 1.5 17. 0.0 0.0 -0. 17. 8.2 10 50 1.9 24- 0 83 10 00 00 86 1E 0.2 1.2 0 02 86 93 00 01 99 -14 3 G 8 1 8 09 1.9 17. 0.0 0.0 -0. 17. 2.9 10 50 2.6 24- 0 90 11 00 00 97 4E 0.4 3.8 5 02 51 79 00 02 75 -14 6 H 4 5 3 09 2.6 17. 0.0 0.0 -0. 18. 2.1 10 50 1.8 24- 0 95 10 00 00 13 3E 1.0 7.6 3 02I 76 15 00 06 41 -14 9 8 0 6 09 3.5 17. 0.0 0.0 -0. 17. 3.1 10 49 1.1 24- 0 69 11 00 00 72 2E 0.2 7.7 0 02 37 42 85 01 72 -14 3 J 9 2 4 09 4.2 17. 0.0 0.0 -0. 17. 2.2 10 50 2.0 24- 1 95 11 00 00 99 8E 0.2 4.4 8 02 83 07 00 01 97 -14 1 K 0 4 5 09 5.0 17. 0.0 0.0 -0. 17. 3.7 10 50 2.1 24- 0 86 10 00 00 94 2E 0.4 3.0 2 02 29 48 00 02 21 -14 0 L 7 7 2 09 0.2 15. 0.0 0.0 -0. 18. 9.1 12 52 16. 24- 0 35 03 00 01 70 1E 1.8 1.6 76 03 95 29 00 13 70 -16 2 A 0 3 9 09 0.3 18. 0.0 0.0 0.0 17. 3.8 97. 49 5.8 24- 5 10 10 00 01 62 4E 3 5.1 8 03 43 02 00 64 02 -15 1 B 9 8 09 0.6 18. 0.0 0.0 0.0 18. 2.0 98. 51 2.4 24- 0 79 11 00 00 51 4E 5 7.0 5 03 32 22 00 93 85 -14 5 C 1 8 09 0.8 18. 0.0 0.0 0.0 18. 5.5 99. 50 1.2 24- 0 21 10 00 00 15 5E 7 8.1 0 03 07 80 00 20 19 -14 2 D 1 1 09 1.0 17. 0.0 0.0 -0. 18. 3.5 10 50 1.6 24- 0 97 09 00 00 04 8E 0.4 5.5 3 03 44 52 00 02 43 -14 0 E 9 4 4 09 1.2 17. 0.0 0.0 0.0 17. 2.2 99. 49 1.5 24- 0 60 11 00 00 46 3E 2 1.3 1 03 93 62 00 48 69 -14 3 F 6 1 09 1.8 17. 0.0 0.0 0.0 17. 1.7 99. 49 1.9 24- 0 64 10 00 00 59 6E 7 4.5 8 03 56 88 00 16 89 -14 8 G 8 8 09 2.6 17. 0.0 0.0 -0. 17. 2.1 10 50 2.2 24- 0 82 10 00 00 88 0E 0.3 1.5 7 03 51 67 00 02 40 -14 8 H 1 0 2 09 3.5 17. 0.0 0.0 -0. 17. 2.5 10 50 2.0 24- 0 79 10 00 00 83 1E 0.2 0.4 4 03I 91 17 00 01 63 -14 1 4 3 6 09 5.0 18. 0.0 0.0 0.0 18. 2.2 99. 50 1.3 24- 0 12 11 00 00 05 5E 6 5.6 0 03 93 35 87 27 03 -14 4 J 1 2 C mu 09 0.2 37. 0.0 0.0 0.0 19. 8.4 51. 54 46. A sco 27- 0 82 09 00 61 54 4E 7 1.8 84 R1 vit 01 15 71 00 85 53 -16 0 e A 9 2 09 0.3 31. 0.0 0.0 0.0 17. 1.9 55. 49 20. 27- 2 87 20 14 47 72 8E 6 7.7 35 01 49 98 56 87 86 -15 7 B 4 3 09 0.5 19. 0.0 0.0 0.0 18. 1.0 94. 52 3.4 27- 0 75 10 00 03 71 3E 7 1.9 7 01 92 81 00 52 97 -14 2 C 6 6 09 0.7 18. 0.0 0.0 0.0 18. 6.4 99. 52 1.2 27- 0 87 10 00 00 78 0E 5 3.5 8 01 77 45 00 30 78 -14 7 D 2 6 09 0.9 19. 0.0 0.0 0.0 18. 1.0 99. 52 1.0 27- 0 04 11 00 00 95 5E 5 7.5 8 01 19 15 00 30 30 -13 6 E 8 9 09 1.2 18. 0.0 0.0 0.0 18. 1.0 99. 52 0.9 27- 0 82 10 00 00 80 6E 9 3.9 5 01 61 66 00 07 38 -13 6 F 4 2 09 1.5 18. 0.0 0.0 -0. 18. 4.9 10 52 0.9 27- 0 63 10 00 00 67 1E 0.2 0.9 9 01 88 47 00 01 87 -14 3 G 8 4 4 09 1.9 18. 0.0 0.0 -0. 18. 2.1 10 52 1.6 27- 0 70 09 00 00 89 4E 1.0 6.1 1 01 71 21 00 06 53 -14 7 H 3 4 2 09 2.4 18. 0.0 0.0 0.0 18. 1.7 99. 51 2.2 27- 0 47 10 00 00 42 6E 8 4.8 3 01I 29 66 00 15 67 -14 1 7 0 09 3.2 18. 0.0 0.0 0.0 18. 7.5 96. 51 5.1 27- 0 88 12 00 02 28 3E 8 1.4 2 01 83 49 00 03 67 -15 1 J 7 0 09 4.2 19. 0.0 0.0 0.0 18. 4.9 99. 52 4.7 27- 1 00 11 00 00 83 3E 1 4.6 6 01 89 72 00 60 20 -15 4 K 5 1 09 5.0 19. 0.0 0.0 -0. 19. 2.0 10 53 4.4 27- 1 33 09 00 00 37 3E 0.2 7.6 0 01 69 36 00 01 25 -14 6 L 0 2 5 09 0.2 19. 0.0 0.0 0.0 12. 2.1 62. 35 89. 27- 0 68 26 00 25 29 5E 5 9.3 94 02 75 49 00 01 67 -16 1 A 2 1 09 0.3 19. 0.0 0.0 0.0 15. 6.9 82. 45 25. 27- 5 22 20 00 11 89 9E 6 2.0 11 02 68 90 00 29 00 -16 8 B 9 9 09 0.5 19. 0.0 0.0 -0. 19. 6.6 10 53 4.6 27- 5 11 08 00 00 18 9E 0.4 3.1 1 02 72 58 00 02 37 -15 2 C 4 3 4 09 0.7 19. 0.0 0.0 -0. 19. 2.9 10 54 4.4 27- 0 54 10 00 00 55 8E 0.0 1.9 1 02 73 01 00 00 01 -14 2 D 6 1 6 09 0.9 19. 0.0 0.0 -0. 19. 1.0 10 53 2.6 27- 0 21 11 00 00 22 5E 0.1 4.1 8 02 36 38 00 00 64 -13 5 E 0 5 1 09 1.3 19. 0.0 0.0 -0. 19. 2.2 10 53 4.3 27- 0 41 10 00 00 41 3E 0.0 8.7 6 02 50 30 00 00 80 -13 5 F 6 1 5 09 1.7 18. 0.0 0.0 0.0 18. 6.4 10 52 1.3 27- 0 88 11 00 00 88 0E 0.0 5.9 0 02 50 15 00 00 39 -14 0 G 1 8 09 2.2 18. 0.0 0.0 0.0 18. 2.1 99. 51 1.2 27- 1 36 10 00 00 34 9E 9 2.8 8 02 92 89 00 07 67 -14 7 H 5 2 09 2.7 18. 0.0 0.0 0.0 18. 8.2 98. 51 3.1 27- 0 76 12 00 01 42 8E 2 4.8 6 02I 42 62 00 14 75 -15 4 6 9 09 3.2 19. 0.0 0.0 -0. 19. 6.0 10 54 3.7 27- 0 24 09 00 00 80 9E 3.0 8.1 3 02 01 11 00 19 99 -15 3 J 2 3 8 09 4.2 19. 0.0 0.0 -0. 19. 1.6 10 54 1.6 27- 1 44 09 00 00 75 8E 1.6 6.7 8 02 15 92 00 10 18 -14 4 K 2 5 8 09 5.0 19. 0.0 0.0 -0. 19. 2.3 10 54 2.4 27- 0 45 09 00 00 62 3E 0.9 3.6 4 02 00 34 00 05 32 -14 7 L 8 9 2 09 0.2 19. -0. 0.0 0.0 18. 5.1 94. 52 36. 27- 5 92 00 00 03 77 4E 3 3.3 24 03 11 21 00 86 92 -16 6 A 9 0 9 09 0.4 19. 0.0 0.0 -0. 19. 2.3 10 54 8.5 27- 5 59 01 00 00 72 1E 0.6 6.0 8 03 50 26 00 04 11 -15 1 B 1 3 0 09 0.7 19. 0.0 0.0 0.0 19. 1.4 99. 54 2.0 27- 0 85 09 00 00 72 3E 4 6.0 5 03 02 62 00 43 28 -14 5 C 0 0 09 0.9 19. 0.0 0.0 0.0 19. 7.4 99. 53 4.3 27- 0 27 09 00 00 20 2E 6 3.5 8 03 89 81 00 26 06 -14 3 D 8 7 09 1.2 18. 0.0 0.0 0.0 18. 1.5 99. 51 5.3 27- 0 59 10 00 00 58 0E 9 8.6 3 03 70 98 00 04 42 -13 4 E 3 1 09 1.6 18. 0.0 0.0 0.0 18. 7.3 10 52 1.5 27- 0 79 11 00 00 79 0E 0.0 3.8 9 03 76 06 00 00 74 -14 0 F 6 2 09 2.1 18. 0.0 0.0 -0. 18. 2.9 10 51 1.3 27- 1 58 10 00 00 60 1E 0.1 9.1 2 03 18 62 00 00 33 -14 0 G 8 7 2 09 2.9 18. 0.0 0.0 0.0 18. 9.0 98. 51 2.9 27- 0 77 10 00 00 52 7E 7 7.1 2 03 20 47 00 84 36 -15 7 H 1 1 09 3.8 19. 0.0 0.0 0.0 19. 3.9 99. 53 5.5 27- 1 42 09 00 00 23 9E 0 4.3 7 03I 09 10 00 63 27 -15 0 8 7 09 5.0 19. 0.0 0.0 0.0 19. 1.6 99. 53 2.2 27- 0 49 10 00 00 43 8E 7 9.2 0 03 11 15 00 17 96 -14 7 J 1 8 M mu 09 0.2 81. 0.0 0.1 0.0 68. 5.5 84. 14 17. R7 sco 28- 0 49 29 14 43 66 8E 3 47. 29 2 vit 01 03 90 49 44 75 -15 41 e A 4 3 09 0.3 30. 0.0 0.0 0.0 24. 4.7 79. 65 8.3 28- 2 68 16 10 21 31 8E 2 2.4 5 01 52 06 40 57 08 -15 5 B 3 0 09 0.5 20. 0.0 0.0 0.0 19. 7.5 92. 53 3.7 28- 0 88 10 00 05 40 9E 9 8.4 5 01 92 98 00 02 43 -15 2 C 2 9 09 0.7 19. 0.0 0.0 0.0 18. 1.0 97. 52 4.9 28- 0 14 10 01 01 70 4E 7 1.6 6 01 82 55 31 49 79 -14 4 D 7 3 09 0.9 18. 0.0 0.0 0.0 17. 1.3 94. 49 3.3 28- 0 88 11 10 03 77 6E 2 8.9 9 01 13 42 93 74 65 -14 4 E 2 9 09 1.1 22. 0.0 0.0 0.0 21. 3.7 98. 59 5.1 28- 1 28 10 04 01 89 5E 2 7.0 5 01 66 65 40 34 01 -14 9 F 4 0 09 1.4 17. 0.0 0.0 0.0 17. 5.0 98. 49 1.6 28- 0 93 10 07 00 74 6E 9 8.2 7 01 62 08 12 64 65 -14 1 G 7 6 09 1.9 18. 0.0 0.0 0.0 18. 4.8 99. 51 3.0 28- 0 50 09 04 00 42 8E 6 4.8 9 01 15 10 12 25 65 -14 1 H 6 9 09 2.5 19. 0.0 0.0 0.0 18. 2.3 98. 52 2.4 28- 0 19 10 10 01 84 9E 2 5.0 9 01I 78 90 76 18 96 -14 7 5 5 09 3.2 19. 0.0 0.0 0.0 19. 6.4 97. 53 3.7 28- 0 73 10 12 01 24 5E 5 4.5 3 01 03 71 41 66 11 -15 0 J 4 2 09 4.2 25. 0.0 0.0 0.0 25. 1.2 97. 67 4.9 28- 2 97 11 63 02 23 2E 1 3.1 6 01 72 37 21 53 54 -14 5 K 2 5 09 5.0 47. 0.0 0.0 0.0 46. 9.3 98. 10 7.6 28- 0 25 11 58 02 66 2E 8 96. 9 01 01 13 84 01 31 -15 43 L 6 4 09 3.0 12 -0. 0.0 -0. 13 7.9 10 22 99. 28- 0 8.8 04 00 02 4.8 5E 4.6 16. 14 01 96 51 00 01 57 -16 74 M 40 5 8 90 09 0.2 10. -0. 0.0 0.0 8.5 6.3 77. 25 19. 28- 0 99 00 00 08 24 2E 5 6.5 75 02 44 08 00 36 69 -16 0 A 2 5 09 0.3 16. 0.0 0.0 0.0 14. 3.4 90. 42 6.1 28- 5 31 10 37 05 71 1E 2 2.2 1 02 71 99 02 44 24 -15 0 B 2 8 09 0.5 18. 0.0 0.0 0.0 17. 1.3 97. 49 2.5 28- 5 16 11 04 01 73 5E 6 7.8 3 02 05 07 44 45 05 -14 1 C 8 3 09 0.8 18. 0.0 0.0 0.0 18. 3.8 98. 51 2.3 28- 0 62 10 02 01 31 3E 3 2.0 5 02 44 42 97 05 38 -14 7 D 2 8 09 1.1 18. 0.0 0.0 0.0 18. 2.3 99. 51 1.0 28- 0 39 10 01 00 36 7E 8 3.3 1 02 92 66 46 12 43 -13 0 E 5 1 09 1.4 18. 0.0 0.0 0.0 18. 1.7 10 50 0.9 28- 0 22 11 01 00 22 3E 0.0 9.9 5 02 64 10 32 00 62 -13 4 F 9 3 09 1.9 18. 0.0 0.0 -0. 18. 2.1 10 51 1.4 28- 0 39 10 00 00 45 2E 0.4 5.5 9 02 20 01 00 02 68 -14 5 G 5 2 6 09 2.4 18. 0.0 0.0 -0. 18. 1.5 10 52 3.7 28- 1 61 10 00 00 83 9E 1.2 4.6 5 02 05 01 00 07 36 -14 8 H 6 6 8 09 2.9 18. 0.0 0.0 0.0 18. 1.6 99. 50 3.0 28- 0 26 11 00 00 21 2E 7 9.6 2 02I 81 18 00 18 31 -14 2 8 2 09 3.5 18. 0.0 0.0 0.0 17. 8.2 98. 50 3.1 28- 0 18 10 00 00 89 6E 4 1.9 6 02 48 73 00 97 79 -15 2 J 3 0 09 4.3 18. 0.0 0.0 0.0 18. 9.4 99. 50 2.6 28- 1 35 10 01 00 21 8E 2 9.6 8 02 97 49 05 49 46 -15 5 K 5 6 09 5.0 18. 0.0 0.0 -0. 18. 1.7 10 51 3.2 28- 1 49 09 00 00 55 0E 0.4 8.0 1 02 19 73 00 02 87 -14 2 L 7 3 0 M mu 09 0.2 14. 0.0 0.0 0.0 9.5 2.7 64. 28 7.9 R7 sco 28- 0 76 15 58 17 19 1E 5 4.1 5 2 vit 03 93 95 51 78 16 -15 8 e A 1 09 0.3 19. 0.0 0.0 0.0 17. 7.7 90. 49 4.1 28- 5 40 14 36 06 45 5E 0 1.1 0 03 32 49 19 59 98 -15 6 B 6 6 09 0.6 19. 0.0 0.0 0.0 18. 2.3 94. 51 1.5 28- 0 65 11 19 03 57 5E 5 8.4 2 03 72 24 30 66 59 -14 4 C 5 7 09 0.9 18. 0.0 0.0 0.0 18. 1.8 99. 51 3.7 28- 0 39 10 03 00 28 5E 4 1.4 2 03 40 29 24 35 92 -13 7 D 5 9 09 1.2 18. 0.0 0.0 -0. 18. 1.3 10 50 2.5 28- 0 05 09 03 00 06 3E 0.1 6.0 0 03 23 73 32 00 52 -13 1 E 9 4 0 09 1.5 18. 0.0 0.0 -0. 18. 6.2 10 51 2.3 28- 0 28 11 03 00 30 4E 0.1 1.7 3 03 69 91 73 00 15 -14 7 F 6 5 3 09 2.0 18. 0.0 0.0 0.0 18. 3.0 10 51 1.6 28- 1 27 10 06 00 27 5E 0.0 1.0 7 03 89 17 61 02 22 -14 6 G 4 7 09 2.8 18. 0.0 0.0 0.0 18. 1.1 99. 50 2.0 28- 0 25 11 26 00 13 0E 4 7.8 6 03 04 47 73 38 92 -14 2 H 3 9 09 3.5 17. 0.0 0.0 0.0 17. 6.8 99. 50 4.0 28- 0 87 12 01 00 82 5E 7 0.1 6 03I 78 07 85 18 36 -15 0 3 3 09 5.0 18. 0.0 0.0 0.0 18. 3.1 99. 51 1.1 28- 1 45 12 20 00 32 3E 3 2.2 7 03 60 13 35 46 04 -14 3 J 9 2 M mu 09 0.2 12. -0. 0.0 -0. 17. 2.2 14 49 50. N8 sco 29- 0 31 00 02 01 44 3E 1.6 0.7 09 5 vit 01 53 68 12 73 37 -16 6 e A 2 0 6 3 09 0.3 12. 0.0 0.0 -0. 14. 3.6 11 41 31. 29- 2 16 06 00 00 55 7E 9.6 8.1 67 01 91 33 00 80 23 -16 0 B 2 7 9 09 0.5 17. 0.0 0.0 0.0 14. 1.4 85. 42 11. 29- 0 47 14 00 08 91 4E 3 7.2 49 01 21 38 00 67 02 -15 5 C 9 6 09 0.7 20. 0.0 0.0 0.0 18. 3.9 93. 52 5.9 29- 0 00 14 02 04 77 0E 8 3.2 6 01 68 06 04 17 34 -15 2 D 4 3 09 0.9 20. 0.0 0.0 0.0 20. 1.3 96. 56 4.0 29- 0 98 10 00 02 31 9E 8 0.1 5 01 80 94 00 28 47 -14 3 E 5 3 09 1.2 20. 0.0 0.0 0.0 20. 1.0 99. 55 1.5 29- 0 20 10 00 00 11 0E 6 5.3 3 01 35 82 84 30 40 -13 7 F 0 1 09 1.6 19. 0.0 0.0 0.0 19. 2.1 99. 55 1.1 29- 0 95 10 00 00 94 3E 9 1.3 1 01 98 54 33 05 47 -13 4 G 1 5 09 2.0 19. 0.0 0.0 0.0 19. 3.3 99. 53 1.3 29- 1 45 10 03 00 40 3E 7 8.5 6 01 87 83 26 17 88 -14 3 H 7 7 09 2.5 18. 0.0 0.0 0.0 18. 2.6 99. 52 3.8 29- 0 91 10 00 00 83 5E 6 4.7 2 01I 34 66 72 26 54 -14 2 2 8 09 3.0 19. 0.0 0.0 -0. 19. 9.5 10 54 3.8 29- 0 37 12 00 00 50 9E 0.7 0.8 0 01 27 07 00 04 71 -15 9 J 3 6 6 09 4.2 19. 0.0 0.0 0.0 19. 8.2 98. 53 3.7 29- 1 83 11 00 01 45 5E 1 9.6 0 01 55 08 74 29 47 -15 3 K 5 2 09 5.0 19. 0.0 0.0 -0. 19. 8.1 10 55 3.8 29- 0 93 09 00 00 94 9E 0.1 1.4 8 01 27 66 00 00 75 -14 1 L 6 5 7 09 0.2 9.4 0.0 0.0 0.0 8.8 5.7 94. 26 18. 29- 0 06 08 00 01 76 5E 4 6.3 20 02 00 49 00 79 96 -16 5 A 09 0.3 16. 0.0 0.0 0.0 15. 2.0 96. 45 9.3 29- 5 50 10 00 02 84 6E 0 0.9 4 02 13 24 00 23 29 -15 0 B 7 5 09 0.5 20. 0.0 0.0 0.0 19. 6.3 95. 53 4.3 29- 5 17 12 00 03 17 9E 0 2.8 8 02 66 71 00 40 11 -15 2 C 6 6 09 0.8 19. 0.0 0.0 0.0 19. 3.3 99. 54 2.7 29- 0 96 10 01 00 82 4E 3 8.5 2 02 72 56 37 47 74 -14 4 D 7 1 09 1.0 19. 0.0 0.0 0.0 19. 1.0 99. 54 1.9 29- 0 70 11 00 00 64 7E 7 4.1 2 02 58 15 00 20 52 -13 9 E 9 4 09 1.3 19. 0.0 0.0 0.0 19. 1.2 10 54 1.3 29- 0 63 11 00 00 63 0E 0.0 3.9 3 02 61 01 00 00 45 -13 4 F 2 1 09 1.7 19. 0.0 0.0 0.0 19. 5.8 99. 53 1.2 29- 0 43 10 00 00 40 3E 8 8.3 5 02 58 87 00 11 26 -14 8 G 3 1 09 2.3 18. 0.0 0.0 0.0 18. 5.0 99. 52 1.3 29- 1 95 11 00 00 92 7E 9 6.9 5 02 20 00 37 08 77 -14 5 H 7 6 09 3.0 19. 0.0 0.0 -0. 19. 1.8 10 53 3.2 29- 1 28 10 22 00 39 7E 0.6 8.1 4 02I 41 21 26 03 34 -14 6 3 7 1 09 4.4 19. 0.0 0.0 0.0 19. 9.9 99. 54 3.2 29- 1 60 11 00 00 57 9E 8 2.4 7 02 36 47 00 10 24 -15 5 J 5 3 09 5.0 20. 0.0 0.0 0.0 20. 7.4 10 55 2.1 29- 0 03 11 44 00 03 4E 0.0 3.4 2 02 18 09 08 01 23 -14 2 K 9 0 09 0.2 19. 0.0 0.1 0.0 13. 3.6 70. 39 7.4 29- 5 01 16 04 18 47 6E 9 0.2 9 03 76 05 04 78 61 -15 9 A 4 5 09 0.4 20. 0.0 0.0 0.0 18. 6.2 91. 51 4.7 29- 0 08 12 11 05 42 2E 7 4.8 9 03 90 56 26 63 62 -15 0 B 0 1 09 0.6 20. 0.0 0.0 0.0 18. 2.4 93. 52 2.2 29- 0 05 11 10 04 81 4E 8 4.1 0 03 96 07 86 23 08 -14 3 C 1 1 09 0.9 18. 0.0 0.0 0.0 18. 1.2 99. 52 1.9 29- 0 86 09 02 00 77 8E 5 3.2 8 03 79 61 98 31 55 -13 7 D 4 0 09 1.2 18. 0.0 0.0 0.0 18. 7.0 99. 52 1.2 29- 0 83 10 02 00 79 8E 8 3.6 4 03 00 50 85 13 03 -14 3 E 2 4 09 1.6 18. 0.0 0.0 -0. 18. 1.9 10 52 1.5 29- 0 70 10 00 00 79 4E 0.5 3.8 2 03 81 54 00 03 85 -14 3 F 4 1 4 09 2.2 18. 0.0 0.0 0.0 18. 1.3 99. 52 2.1 29- 1 87 11 00 00 74 6E 3 2.4 4 03 29 34 00 45 01 -14 2 G 9 0 09 3.3 18. 0.0 0.0 0.0 18. 6.0 99. 51 4.9 29- 1 70 10 00 00 59 9E 4 9.0 1 03 79 89 00 36 98 -15 2 H 9 9 09 4.5 19. 0.0 0.0 0.0 19. 1.9 99. 53 1.5 29- 1 53 11 03 00 37 9E 2 7.7 3 03I 38 87 28 53 55 -14 3 2 3 09 5.0 19. 0.0 0.0 -0. 19. 6.3 10 55 3.8 29- 0 53 09 00 00 99 2E 2.3 2.4 0 03 59 60 00 15 10 -15 4 J 3 4 1 FD mu 09 0.2 23. 0.0 0.5 0.0 -0. 1.9 -1. -12 16 A sco 31- 0 65 57 48 81 37 9E 6 .10 2.0 vit 01 92 39 60 47 28 -16 9 e A 4 3 09 0.3 28. 0.0 0.0 0.0 11. 2.6 39. 33 12 31- 2 77 71 00 58 37 0E 5 4.7 2.1 01 18 22 00 86 72 -16 8 1 B 4 4 09 0.5 18. 0.0 0.0 0.0 11. 4.3 61. 33 44. 31- 0 83 32 27 24 56 3E 4 9.9 56 01 29 24 26 58 99 -16 5 C 4 8 09 0.7 20. 0.0 0.0 0.0 15. 1.6 74. 43 14. 31- 0 67 19 33 17 39 0E 5 9.6 31 01 17 98 66 86 57 -15 0 D 0 0 09 0.9 18. 0.0 0.0 0.0 17. 4.7 90. 48 4.4 31- 0 89 14 00 06 10 5E 6 2.5 6 01 05 20 00 03 91 -15 0 E 8 6 09 1.1 18. 0.0 0.0 0.0 17. 1.3 96. 49 2.2 31- 1 19 11 00 02 52 7E 3 2.7 8 01 77 17 00 28 36 -14 3 F 0 8 09 1.4 17. 0.0 0.0 0.0 17. 5.4 99. 49 1.5 31- 0 71 11 00 00 67 6E 8 6.4 7 01 20 01 00 12 55 -14 7 G 0 8 09 1.8 17. 0.0 0.0 0.0 17. 1.6 99. 49 3.6 31- 0 66 10 00 00 64 0E 9 5.7 5 01 51 89 00 06 69 -13 6 H 3 4 09 2.4 17. 0.0 0.0 -0. 17. 3.2 10 50 1.1 31- 0 89 10 00 00 95 4E 0.3 3.3 5 01I 64 75 00 02 73 -14 7 2 1 3 09 3.0 17. 0.0 0.0 -0. 17. 1.3 10 49 2.5 31- 1 59 10 00 00 67 6E 0.5 6.5 7 01 06 15 00 03 75 -14 1 J 4 0 0 09 4.3 17. 0.0 0.0 0.0 17. 1.2 99. 48 4.0 31- 1 51 10 00 00 40 0E 4 9.8 0 01 27 98 00 36 46 -14 0 K 3 1 09 5.0 17. 0.0 0.0 0.0 17. 1.6 99. 49 2.4 31- 0 63 10 00 00 58 8E 7 4.1 6 01 97 34 00 19 26 -14 8 L 4 4 FD mu 09 0.2 31. 0.0 0.4 0.1 -0. 2.5 -2. -27 17 A sco 31- 5 94 86 37 11 83 0E 6 .11 3.4 vit 02 17 72 21 02 22 -16 0 e A 0 7 09 0.4 19. -0. 0.1 -0. 20. 2.5 10 57 62. 31- 0 11 01 53 00 80 4E 8.8 1.7 47 02 62 04 93 56 77 -16 8 B 5 6 8 9 09 0.6 34. 0.0 1.5 0.0 15. 1.8 45. 44 24. 31- 5 26 28 53 63 49 2E 2 2.1 12 02 53 65 09 99 55 -15 3 C 4 3 09 0.9 20. 0.0 0.1 0.0 17. 4.5 84. 48 6.7 31- 0 61 12 02 11 31 9E 0 7.5 1 02 94 55 79 22 15 -15 0 D 0 6 09 1.2 19. 0.0 0.0 0.0 17. 1.7 92. 49 2.2 31- 0 00 11 00 04 65 6E 9 6.0 1 02 58 76 00 55 99 -14 8 E 8 5 09 1.6 17. 0.0 0.0 0.0 17. 1.2 99. 49 1.5 31- 0 76 11 00 00 64 4E 3 5.5 4 02 40 18 33 42 01 -13 9 F 6 0 09 2.2 17. 0.0 0.0 0.0 17. 3.3 99. 49 1.1 31- 1 64 10 00 00 60 9E 8 4.6 7 02 54 48 15 14 23 -13 7 G 8 6 09 3.0 17. 0.0 0.0 0.0 17. 2.7 99. 48 1.9 31- 1 44 10 02 00 28 8E 1 6.8 3 02 47 79 49 54 50 -14 5 H 8 9 09 4.2 17. 0.0 0.0 0.0 17. 3.4 10 49 1.9 31- 2 68 10 00 00 67 3E 0.0 6.4 6 02I 38 09 00 03 47 -14 5 0 9 09 5.0 17. 0.0 0.0 -0. 17. 5.1 10 49 1.2 31- 0 71 10 00 00 72 8E 0.0 7.6 1 02 83 97 00 00 26 -14 2 J 5 2 9 09 0.2 22. -0. 0.0 0.0 18. 4.2 81. 51 49. 31- 5 39 03 00 13 27 7E 6 1.0 06 03 33 33 00 94 31 -16 8 A 4 0 8 09 0.4 17. -0. 0.0 -0. 18. 5.8 10 51 25. 31- 0 43 00 00 00 56 2E 6.5 8.0 16 03 62 32 00 38 13 -16 8 B 2 6 1 2 09 0.6 19. 0.0 0.0 0.0 17. 1.9 91. 49 10. 31- 0 38 12 00 05 66 9E 1 6.1 75 03 34 46 00 82 29 -15 5 C 4 2 09 0.8 23. 0.0 0.0 0.0 17. 6.9 75. 49 5.4 31- 0 56 14 04 19 77 1E 4 8.8 5 03 73 71 34 61 32 -15 6 D 2 0 09 1.0 18. 0.0 0.0 0.0 17. 5.6 96. 49 1.1 31- 0 27 11 00 02 60 6E 4 4.7 3 03 23 28 00 26 48 -14 3 E 2 1 09 1.3 17. 0.0 0.0 0.0 17. 2.0 10 49 0.7 31- 0 60 10 00 00 60 5E 0.0 4.6 1 03 05 93 00 00 09 -13 3 F 3 2 09 1.8 17. 0.0 0.0 0.0 17. 1.0 99. 49 1.4 31- 0 75 10 00 00 65 5E 4 5.8 3 03 35 46 00 34 11 -13 6 G 7 1 09 2.5 17. 0.0 0.0 0.0 17. 2.7 99. 49 2.2 31- 0 83 11 00 00 81 6E 9 9.9 1 03 49 32 00 05 86 -13 7 H 6 0 09 3.6 17. 0.0 0.0 -0. 17. 1.0 10 50 1.0 31- 1 84 11 00 00 85 1E 0.0 0.7 8 03I 47 48 00 00 14 -13 8 3 3 2 09 5.0 17. 0.0 0.0 0.0 17. 3.6 99. 49 3.7 31- 0 81 09 00 00 71 0E 5 7.5 8 03 58 70 00 33 89 -14 3 J 0 7 FD bi- 09 0.2 17. 0.0 0.0 0.0 4.3 5.3 25. 13 41. A otit 32- 0 21 18 97 43 72 5E 4 6.1 10 e 01 26 96 90 48 39 -16 1 A 4 09 0.3 9.5 0.0 0.0 0.0 6.9 1.6 72. 21 7.2 32- 2 84 15 30 08 38 5E 4 1.4 8 01 65 05 67 96 32 -15 4 B 09 0.5 17. 0.0 0.0 0.0 16. 1.9 95. 47 2.7 32- 0 67 12 01 02 94 6E 8 8.4 8 01 99 03 23 49 48 -14 3 C 6 1 09 0.7 17. 0.0 0.0 0.0 17. 5.4 99. 48 1.6 32- 0 53 10 00 00 36 1E 0 8.8 5 01 83 96 00 58 63 -14 6 D 4 5 09 0.9 17. 0.0 0.0 0.0 17. 4.6 99. 49 2.6 32- 0 50 09 00 00 46 5E 8 1.2 6 01 50 32 00 14 30 -14 4 E 5 4 09 1.2 18. 0.0 0.0 0.0 17. 6.6 99. 50 1.8 32- 0 04 10 00 00 94 8E 4 3.0 3 01 53 82 00 35 20 -14 0 F 4 4 09 1.5 17. 0.0 0.0 0.0 17. 7.6 99. 50 1.0 32- 0 93 10 00 00 91 8E 9 2.4 0 01 09 56 00 04 84 -14 2 G 6 2 09 1.9 17. 0.0 0.0 0.0 17. 6.0 99. 49 1.1 32- 0 84 11 00 00 80 0E 8 9.5 4 01 50 61 00 15 02 -14 2 H 2 9 09 2.4 17. 0.0 0.0 0.0 17. 3.8 99. 49 1.4 32- 0 68 10 00 00 58 4E 5 4.2 4 01I 26 48 00 32 70 -14 9 4 6 09 3.2 17. 0.0 0.0 -0. 17. 1.5 10 50 1.8 32- 0 73 09 00 00 84 7E 0.6 0.6 2 01 98 46 00 03 41 -14 0 J 2 6 1 09 4.3 17. 0.0 0.0 -0. 19. 2.3 11 55 7.0 32- 1 85 05 00 00 96 0E 1.9 1.8 1 01 04 28 00 71 58 -15 4 K 4 6 5 09 5.0 17. 0.0 0.0 -0. 17. 2.0 10 50 1.4 32- 0 78 09 00 00 94 3E 0.9 3.1 8 01 27 59 00 05 68 -14 1 L 7 6 3 09 0.2 7.2 0.0 0.0 0.0 5.8 6.5 80. 17 12. 32- 5 44 01 00 04 16 3E 3 8.9 05 02 99 87 00 83 71 -16 0 A 09 0.4 16. 0.0 0.0 0.0 15. 6.0 94. 43 3.3 32- 0 10 11 04 02 25 5E 7 5.9 9 02 41 02 03 89 12 -15 3 B 8 4 09 0.6 17. 0.0 0.0 0.0 17. 6.9 99. 49 1.4 32- 5 74 11 01 00 58 8E 1 4.1 4 02 41 67 46 54 29 -14 9 C 9 7 09 0.9 17. 0.0 0.0 -0. 17. 9.0 10 50 1.5 32- 0 86 10 00 00 88 1E 0.1 1.6 7 02 54 36 00 00 80 -14 8 D 2 8 6 09 1.2 17. 0.0 0.0 0.0 17. 8.4 99. 49 1.6 32- 0 76 11 00 00 72 6E 8 7.7 2 02 79 08 62 13 94 -14 9 E 7 0 09 1.5 17. 0.0 0.0 0.0 17. 8.4 99. 50 1.2 32- 0 98 11 01 00 95 8E 8 3.4 1 02 67 90 45 09 89 -14 1 F 4 7 09 1.9 18. 0.0 0.0 0.0 18. 1.0 10 50 1.9 32- 0 03 10 00 00 02 0E 0.0 4.9 2 02 15 36 00 03 33 -13 8 G 5 0 09 2.7 17. 0.0 0.0 0.0 17. 1.0 99. 50 0.8 32- 0 86 10 00 00 84 5E 9 0.6 3 02 02 79 00 04 68 -13 6 H 6 0 09 3.8 17. 0.0 0.0 0.0 17. 7.7 99. 49 2.7 32- 1 75 10 00 00 74 0E 9 8.1 8 02I 56 67 00 03 56 -14 8 8 4 09 5.0 17. 0.0 0.0 0.0 17. 9.8 99. 50 3.8 32- 0 92 10 00 00 83 4E 5 0.4 0 02 29 48 00 28 91 -15 8 J 2 1 09 0.2 10. 0.0 0.0 -0. 10. 1.0 10 32 11. 32- 5 08 08 01 00 96 1E 8.7 3.6 12 03 76 48 40 29 28 -15 2 A 3 6 4 09 0.4 16. -0. 0.0 -0. 25. 6.9 15 68 21. 32- 0 32 01 00 03 97 4E 9.1 9.5 18 03 71 08 00 26 55 -16 5 B 3 9 5 2 09 0.6 17. 0.0 0.0 -0. 17. 4.4 10 50 4.4 32- 5 53 09 00 00 86 0E 1.8 1.0 0 03 81 60 00 11 11 -15 2 C 1 0 1 09 0.9 17. 0.0 0.0 -0. 17. 7.6 10 49 4.2 32- 0 47 10 00 00 51 7E 0.2 2.4 8 03 84 76 00 01 08 -14 2 D 0 1 5 09 1.2 17. 0.0 0.0 -0. 17. 4.5 10 50 2.9 32- 0 73 11 01 00 82 2E 0.5 0.0 9 03 92 23 02 02 32 -14 9 E 7 9 7 09 1.5 17. 0.0 0.0 0.0 17. 5.0 99. 49 3.1 32- 0 76 10 00 00 75 2E 9 8.3 4 03 32 39 41 04 07 -14 1 F 5 7 09 2.0 17. 0.0 0.0 -0. 17. 7.2 10 49 1.8 32- 1 72 10 00 00 75 5E 0.2 8.3 6 03 35 02 85 00 02 -14 0 G 9 9 7 09 2.7 17. 0.0 0.0 0.0 17. 4.5 99. 50 1.2 32- 0 99 10 01 00 96 6E 8 3.5 9 03 67 98 53 10 62 -14 9 H 4 8 09 3.8 17. 0.0 0.0 -0. 17. 3.3 10 50 1.1 32- 1 85 10 00 00 87 6E 0.1 1.3 4 03I 11 62 00 00 65 -14 9 1 9 6 09 5.0 17. 0.0 0.0 0.0 17. 7.3 99. 49 2.7 32- 0 85 11 00 00 81 2E 7 9.7 6 03 84 08 00 16 04 -15 7 J 0 7 SP A0 20 3-7 3 H6 bi- 14 0.4 34. -0. 0.0 0.0 31. 8.5 91. 39 17. 93 otit 85- 0 32 01 00 10 36 7E 4 4.0 90 C e 01 23 26 00 00 17 -16 5 A 0 6 5 14 0.8 47. 0.0 0.0 0.0 47. 4.4 99. 56 1.6 85- 0 92 10 00 00 73 5E 6 9.9 2 01 10 91 00 64 25 -14 7 B 9 7 14 1.2 48. 0.0 0.0 -0. 48. 9.2 10 57 2.1 85- 0 56 10 00 00 57 4E 0.0 8.6 6 01 30 47 00 00 80 -14 1 C 5 5 3 14 1.6 48. 0.0 0.0 -0. 48. 7.0 10 57 1.2 85- 0 08 11 00 00 09 1E 0.0 3.7 4 01 35 22 00 00 93 -14 2 D 2 6 0 14 2.0 48. 0.0 0.0 0.0 47. 5.5 99. 57 1.9 85- 1 03 11 00 00 89 8E 7 1.6 6 01 50 58 00 47 47 -14 3 E 0 4 14 2.5 48. 0.0 0.0 0.0 48. 4.7 99. 57 1.5 85- 0 19 11 00 00 15 4E 9 4.2 2 01 33 64 00 14 11 -14 5 F 5 8 14 3.0 47. 0.0 0.0 0.0 47. 4.5 10 57 1.3 85- 1 97 10 00 00 95 1E 0.0 2.2 3 01 74 93 00 07 54 -14 5 G 0 7 14 3.8 48. 0.0 0.0 -0. 48. 1.2 10 57 1.3 85- 1 24 11 00 00 28 0E 0.1 5.6 2 01 80 36 00 01 28 -13 0 H 3 2 4 14 5.1 48. 0.0 0.0 0.0 48. 1.3 99. 57 1.8 85- 9 44 11 04 00 41 6E 9 6.9 8 01I 01 35 70 10 14 -13 1 9 1 H6 bi- 14 0.6 48. 0.0 0.0 0.0 48. 4.9 99. 57 1.9 93 otit 85- 0 57 09 00 01 06 1E 0 3.3 4 C e 02 02 13 00 72 06 -14 3 A 7 2 14 1.1 48. 0.0 0.0 0.0 48. 9.7 99. 57 1.5 85- 0 65 11 00 00 57 5E 9 8.6 4 02 02 69 00 24 76 -14 0 B 3 4 14 1.6 48. 0.0 0.0 -0. 48. 6.0 10 57 1.7 85- 0 42 11 00 00 44 2E 0.1 7.2 1 02 00 17 00 00 52 -14 5 C 4 9 0 14 2.2 48. 0.0 0.0 0.0 48. 6.0 99. 57 1.4 85- 1 65 11 00 00 52 6E 7 8.0 1 02 33 76 00 43 65 -14 8 D 5 7 14 3.0 48. 0.0 0.0 0.0 48. 8.6 99. 57 1.2 85- 1 73 12 20 00 65 9E 8 9.4 3 02 73 42 62 27 98 -14 4 E 2 5 14 3.7 48. 0.0 0.0 0.0 48. 4.9 99. 58 1.9 85- 1 86 11 16 00 76 1E 8 0.5 1 02 58 97 09 34 57 -14 2 F 5 5 14 4.2 48. 0.0 0.0 -0. 50. 7.7 10 59 3.5 85- 1 72 09 00 00 17 9E 3.0 4.7 8 02 56 79 00 49 36 -15 9 G 1 0 5 14 5.1 49. 0.0 0.0 -0. 52. 2.6 10 61 8.6 85- 9 09 12 96 01 08 0E 6.1 4.0 0 02 40 75 95 00 65 -15 1 H 1 9 2 14 0.6 48. 0.0 0.0 0.0 47. 1.8 97. 56 2.4 85- 0 66 13 59 04 34 3E 3 5.9 6 03 33 90 10 48 43 -14 9 A 5 1 14 1.1 49. 0.0 0.0 0.0 49. 8.8 99. 58 1.5 85- 0 48 12 12 00 30 9E 6 5.9 3 03 73 56 02 62 39 -14 9 B 3 2 14 1.6 49. 0.0 0.0 0.0 49. 8.9 99. 58 1.2 85- 0 39 10 00 00 32 1E 8 6.1 6 03 89 63 00 25 35 -14 9 C 1 0 14 2.2 49. 0.0 0.0 0.0 49. 6.9 99. 58 1.4 85- 1 25 11 62 00 12 7E 7 4.1 7 03 76 66 50 49 06 -14 3 D 8 1 14 3.0 49. 0.0 0.0 0.0 49. 9.4 99. 58 1.9 85- 1 61 11 40 00 43 0E 6 7.3 3 03 53 34 43 61 81 -14 5 E 7 3 14 3.6 49. 0.0 0.0 0.0 49. 8.5 99. 58 1.4 85- 1 44 08 23 00 24 6E 6 5.3 5 03 04 61 52 67 47 -14 9 F 4 3 14 4.2 49. 0.0 0.0 0.0 49. 7.8 99. 58 1.3 85- 1 54 11 00 00 45 2E 8 7.5 1 03 73 29 00 31 39 -14 1 G 4 2 14 5.2 48. 0.0 0.0 -0. 49. 3.9 10 58 1.9 85- 0 79 10 00 00 01 9E 0.4 3.0 2 03 69 71 00 07 56 -14 6 H 2 4 2 H1 bi- 14 0.4 45. 0.0 0.2 0.0 32. 4.9 72. 40 8.4 09 otit 88- 0 16 18 35 42 58 5E 1 7.8 1 e 01 77 57 99 66 51 -15 1 A 3 9 14 0.8 41. 0.0 0.0 0.0 40. 1.0 96. 48 1.0 88- 0 76 13 00 05 09 4E 0 9.9 3 01 31 28 00 66 06 -13 8 B 5 1 14 1.2 40. 0.0 0.0 0.0 40. 9.3 99. 49 0.8 88- 0 33 12 00 00 26 3E 8 1.8 5 01 33 15 00 24 18 -14 1 C 0 8 14 1.6 40. 0.0 0.0 0.0 40. 9.5 99. 49 0.7 88- 0 46 12 00 00 35 2E 7 2.8 9 01 34 23 00 35 88 -14 5 D 5 0 14 2.0 40. 0.0 0.0 0.0 40. 7.8 99. 48 1.3 88- 1 23 11 30 00 08 0E 6 9.9 2 01 72 74 04 53 36 -14 1 E 8 9 14 2.5 40. 0.0 0.0 0.0 40. 5.4 99. 48 2.1 88- 0 12 10 00 00 04 4E 8 9.5 5 01 83 97 00 28 59 -14 0 F 6 7 14 3.0 40. 0.0 0.0 0.0 39. 4.1 99. 48 1.0 88- 1 06 11 00 00 99 3E 8 8.9 4 01 87 63 00 25 29 -14 4 G 6 5 14 4.0 39. 0.0 0.0 0.0 39. 5.1 99. 48 1.2 88- 1 51 11 00 01 21 6E 2 0.5 7 01 14 72 00 01 30 -14 6 H 7 1 14 5.1 39. 0.0 0.0 0.0 39. 4.7 99. 48 2.1 88- 9 29 10 00 00 24 9E 9 0.8 6 01I 81 85 00 18 32 -14 9 7 9 14 0.5 42. 0.0 0.0 0.0 39. 2.0 92. 48 1.9 88- 0 29 12 00 10 18 0E 7 0.2 1 02 05 61 00 51 27 -14 4 A 3 0 14 0.8 39. 0.0 0.0 0.0 39. 7.8 99. 48 1.2 88- 0 75 11 00 00 69 4E 9 5.7 6 02 19 64 00 18 87 -14 8 B 5 8 14 1.2 40. 0.0 0.0 0.0 40. 9.1 99. 48 0.9 88- 0 04 12 00 00 02 9E 9 9.3 0 02 95 36 00 07 70 -14 0 C 1 3 14 1.6 40. 0.0 0.0 0.0 40. 4.9 99. 49 1.2 88- 0 48 12 20 00 34 6E 6 2.6 9 02 81 33 89 50 35 -14 9 D 9 4 14 2.0 40. 0.0 0.0 0.0 40. 5.6 99. 49 1.1 88- 1 19 11 00 00 13 3E 8 0.4 9 02 62 79 00 20 53 -14 6 E 7 4 14 2.8 40. 0.0 0.0 0.0 39. 7.9 99. 48 1.0 88- 0 04 12 00 00 99 0E 9 8.9 1 02 92 38 00 20 11 -14 2 F 9 9 14 4.0 40. 0.0 0.0 0.0 40. 4.0 99. 48 3.0 88- 1 17 11 00 00 07 9E 8 9.8 3 02 40 57 00 32 95 -14 6 G 9 4 14 5.1 39. 0.0 0.0 0.0 39. 1.8 99. 48 2.0 88- 9 40 13 00 00 29 6E 7 1.4 5 02 53 67 00 38 23 -14 2 H 8 7 14 0.5 44. 0.0 0.0 0.0 19. 5.4 44. 25 8.2 88- 0 72 20 00 84 90 3E 5 9.8 8 03 97 59 00 00 49 -15 7 A 7 7 14 0.8 47. 0.0 0.0 0.0 40. 2.8 85. 49 3.2 88- 0 38 15 00 23 35 6E 2 2.7 8 03 74 43 00 81 12 -14 7 B 6 3 14 1.2 43. 0.0 0.0 0.0 39. 1.2 91. 48 1.1 88- 0 43 14 00 12 86 0E 8 7.5 2 03 25 48 00 07 51 -13 7 C 2 3 14 1.6 42. 0.0 0.0 0.0 40. 1.5 94. 48 0.8 88- 0 55 13 00 08 04 0E 1 9.5 4 03 85 90 00 49 84 -13 3 D 3 6 14 2.0 42. 0.0 0.0 0.0 40. 1.3 96. 49 0.8 88- 1 00 12 00 05 32 2E 0 2.4 3 03 55 19 00 69 43 -13 8 E 9 0 14 2.6 40. 0.0 0.0 0.0 40. 1.5 99. 49 0.9 88- 9 55 12 00 00 36 7E 5 2.8 4 03 86 32 00 66 21 -13 8 F 6 7 14 4.0 40. 0.0 0.0 0.0 40. 1.1 99. 49 1.0 88- 1 30 12 00 00 21 9E 8 1.3 1 03 12 16 00 29 36 -13 0 G 7 6 14 5.2 39. 0.0 0.0 0.0 39. 5.5 99. 48 3.1 88- 0 77 11 17 00 59 6E 6 4.6 0 03 13 62 51 61 34 -14 5 H 2 1 H4 bi- 14 0.4 47. 0.0 0.1 0.0 43. 3.4 92. 52 8.0 65 otit 89- 0 35 12 72 12 80 7E 5 9.2 9 e 01 35 15 00 08 09 -15 6 A 3 2 14 0.8 49. 0.0 0.0 0.0 49. 1.7 99. 58 1.2 89- 0 20 11 18 00 05 1E 7 3.5 0 01 92 28 79 51 88 -13 0 B 7 7 14 1.2 49. 0.0 0.0 0.0 49. 1.3 99. 58 1.3 89- 0 57 12 20 00 46 9E 8 7.6 0 01 47 66 54 36 94 -13 7 C 9 8 14 1.6 49. 0.0 0.0 0.0 49. 6.8 99. 58 2.3 89- 0 44 12 01 00 34 0E 8 6.3 2 01 19 98 84 33 37 -14 9 D 7 8 14 2.1 49. 0.0 0.0 0.0 49. 5.8 99. 58 1.4 89- 1 37 11 00 00 26 7E 8 5.5 6 01 31 72 00 37 42 -14 8 E 3 0 14 2.7 49. 0.0 0.0 -0. 49. 6.8 10 58 3.7 89- 0 11 08 00 00 17 8E 0.1 4.6 7 01 94 56 00 01 20 -14 5 F 8 8 0 14 3.3 49. 0.0 0.0 0.0 49. 7.8 99. 58 1.2 89- 1 36 11 00 00 26 1E 8 5.6 0 01 47 87 00 32 85 -14 3 G 9 9 14 4.0 49. 0.0 0.0 -0. 49. 7.8 10 58 1.2 89- 1 33 10 00 00 39 3E 0.1 6.8 8 01 01 30 00 02 18 -14 8 H 6 1 8 14 5.1 49. 0.0 0.0 -0. 49. 4.6 10 59 1.3 89- 9 75 11 00 00 92 8E 0.3 2.2 3 01I 85 01 00 05 35 -14 6 0 6 5 14 0.5 48. 0.0 0.0 0.0 47. 1.2 98. 57 7.5 89- 0 73 10 00 02 93 2E 4 2.0 4 02 53 49 00 71 49 -14 4 A 9 4 14 0.8 49. 0.0 0.0 0.0 49. 8.1 99. 58 1.4 89- 0 68 11 00 00 63 3E 9 9.3 5 02 91 35 00 19 28 -14 2 B 3 9 14 1.2 49. 0.0 0.0 0.0 49. 1.8 99. 58 1.4 89- 0 55 11 00 00 51 6E 9 8.1 9 02 62 61 00 15 19 -13 0 C 1 2 14 1.8 49. 0.0 0.0 -0. 49. 1.4 10 58 1.1 89- 0 54 10 00 00 56 5E 0.0 8.6 1 02 06 61 00 00 42 -13 3 D 3 8 5 14 2.8 49. 0.0 0.0 0.0 49. 1.2 99. 58 1.4 89- 0 54 10 00 00 49 3E 9 7.8 4 02 84 87 00 19 05 -13 8 E 4 5 14 3.7 49. 0.0 0.0 -0. 49. 7.5 10 58 1.5 89- 1 48 11 00 00 58 5E 0.2 8.8 2 02 96 11 00 03 49 -14 4 F 0 2 3 14 5.1 50. 0.0 0.0 0.0 50. 1.5 10 59 2.0 89- 9 45 09 00 00 43 4E 0.0 7.4 5 02 15 48 00 06 36 -13 2 G 0 6 H4 bi- 14 0.6 49. 0.0 0.1 0.0 47. 4.7 96. 57 1.7 65 otit 89- 0 55 12 61 05 98 0E 8 2.5 4 e 03 34 82 96 36 67 -14 7 A 1 6 14 0.9 48. 0.0 0.0 0.0 48. 1.1 99. 57 3.0 89- 0 81 12 35 00 62 5E 6 9.0 6 03 41 42 09 66 24 -13 6 B 7 0 14 1.2 49. 0.0 0.0 0.0 49. 1.2 99. 58 1.2 89- 0 28 11 42 00 14 8E 7 4.4 3 03 27 28 83 47 71 -13 0 C 3 9 14 1.9 49. 0.0 0.0 0.0 49. 1.6 99. 58 2.0 89- 0 60 12 30 00 51 4E 8 8.1 8 03 06 15 56 29 86 -13 7 D 2 0 14 2.8 49. 0.0 0.0 0.0 49. 1.2 10 58 1.1 89- 1 22 11 05 00 21 2E 0.0 5.0 6 03 24 65 25 02 57 -13 9 E 4 8 14 3.8 49. 0.0 0.0 -0. 49. 7.3 10 58 1.9 89- 1 39 10 00 00 51 7E 0.2 8.1 5 03 90 68 00 04 71 -14 5 F 2 0 7 14 5.2 49. 0.0 0.0 -0. 49. 1.3 10 59 1.2 89- 0 71 11 00 00 79 5E 0.2 0.9 2 03 01 48 00 02 39 -13 5 G 4 9 7 H5 mu 14 0.4 34. 0.0 4.5 0.0 14. 5.7 40. 18 32. 59 sco 91- 0 93 47 94 72 01 2E 0 6.8 96 vit 01 99 12 24 19 62 -16 1 e A 5 4 14 0.8 66. 0.0 0.0 0.0 55. 4.3 82. 64 9.8 91- 0 84 11 00 38 34 1E 8 6.3 8 01 29 15 00 89 85 -15 1 B 7 3 14 1.2 52. 0.0 0.0 0.0 50. 1.6 95. 59 2.8 91- 0 89 14 00 08 24 1E 0 5.5 3 01 12 92 00 94 78 -14 4 C 4 3 14 1.6 51. 0.0 0.0 -0. 51. 6.6 10 60 1.8 91- 0 08 10 00 00 10 9E 0.0 4.2 4 01 69 22 00 00 74 -14 0 D 9 7 6 14 2.1 49. 0.0 0.0 0.0 49. 1.5 99. 59 1.0 91- 1 96 11 00 00 85 4E 8 1.6 1 01 87 90 00 37 94 -13 2 E 7 2 14 2.7 49. 0.0 0.0 0.0 49. 2.7 99. 59 1.2 91- 0 92 12 00 00 86 8E 9 1.6 7 01 14 38 00 19 35 -13 6 F 2 6 14 3.3 49. 0.0 0.0 0.0 49. 1.8 99. 58 1.3 91- 1 60 12 18 00 53 5E 9 8.3 8 01 63 45 48 25 48 -13 3 G 2 7 14 4.2 48. 0.0 0.7 0.0 48. 3.4 99. 58 1.4 91- 1 94 11 99 00 92 8E 9 2.1 3 01 52 21 48 38 18 -14 1 H 7 0 14 5.1 49. 0.0 0.0 0.0 49. 1.5 99. 59 1.5 91- 9 91 11 17 00 83 7E 8 1.3 7 01I 29 10 66 27 40 -13 6 4 1 14 1.0 50. 0.0 0.0 0.0 47. 1.0 94. 56 3.0 91- 0 25 13 00 08 67 5E 9 9.3 7 02 86 06 00 74 54 -14 9 A 9 4 14 1.6 49. 0.0 0.0 0.0 49. 1.6 99. 58 1.6 91- 0 67 11 00 00 43 9E 5 7.3 5 02 23 16 00 80 54 -13 2 B 6 5 14 2.1 49. 0.0 0.0 0.0 49. 2.6 99. 58 1.2 91- 1 63 11 00 00 48 4E 7 7.8 2 02 09 90 00 50 25 -13 0 C 5 5 14 2.5 49. 0.0 0.0 0.0 49. 1.6 99. 58 0.9 91- 0 37 12 00 00 28 5E 8 5.7 3 02 56 29 00 31 48 -13 9 D 0 6 14 3.0 49. 0.0 0.0 0.0 49. 1.9 99. 58 1.2 91- 1 38 11 08 00 30 0E 8 6.0 5 02 54 52 24 26 93 -13 4 E 5 3 14 4.3 48. 0.0 0.0 0.0 48. 4.6 99. 57 1.7 91- 1 43 11 00 00 37 0E 9 6.5 7 02 63 94 00 22 21 -14 1 F 9 3 14 5.2 49. 0.0 0.0 0.0 49. 1.5 10 59 1.0 91- 0 80 11 00 00 79 9E 0.0 0.9 5 02 23 77 00 02 60 -13 8 G 0 8 14 1.0 59. 0.0 0.0 0.0 49. 1.6 83. 58 4.4 91- 0 12 22 00 33 09 1E 0 3.8 6 03 56 92 00 95 35 -14 5 A 5 3 14 1.6 50. 0.0 0.0 0.0 49. 1.4 98. 58 1.1 91- 0 13 12 03 02 48 7E 7 7.8 8 03 29 63 70 20 30 -13 0 B 8 6 14 2.0 49. 0.0 0.0 0.0 49. 2.0 99. 58 1.2 91- 0 59 12 00 00 50 8E 8 8.0 1 03 63 18 00 29 99 -13 8 C 2 6 14 2.5 49. 0.0 0.0 0.0 49. 1.6 99. 58 1.1 91- 0 39 11 00 00 29 8E 8 5.9 1 03 72 94 00 34 56 -13 0 D 8 1 14 3.0 48. 0.0 0.0 0.0 47. 3.7 99. 57 1.5 91- 1 23 12 52 01 76 1E 0 0.3 4 03 69 61 84 61 66 -14 2 E 0 2 14 4.3 48. 0.0 0.0 0.0 47. 1.9 98. 56 2.5 91- 1 31 12 00 02 62 2E 6 8.8 3 03 24 34 00 32 66 -14 9 F 7 8 14 5.1 49. 0.0 0.0 0.0 49. 1.0 99. 58 2.0 91- 9 62 11 00 00 57 3E 9 8.7 1 03 64 53 00 18 32 -13 2 G 1 9 H7 bi- 14 0.4 43. 0.0 0.0 0.0 40. 5.3 91. 48 4.7 51 otit 92- 0 65 18 00 12 02 3E 7 9.2 7 e 01 71 33 00 29 52 -15 8 A 7 2 14 0.8 43. 0.0 0.0 0.0 42. 5.5 98. 51 1.3 92- 0 58 13 00 02 71 5E 0 7.8 4 01 60 45 00 96 19 -14 2 B 8 1 14 1.2 42. 0.0 0.0 0.0 42. 8.1 99. 51 1.0 92- 0 86 12 00 00 71 9E 7 7.8 4 01 43 57 00 51 45 -14 5 C 0 4 14 1.6 42. 0.0 0.0 0.0 42. 1.2 99. 51 1.0 92- 0 80 12 00 00 73 3E 8 8.1 7 01 90 97 00 24 90 -13 1 D 4 2 14 2.0 42. 0.0 0.0 -0. 42. 7.2 10 51 0.9 92- 0 50 13 00 00 52 8E 0.0 5.8 5 01 73 14 00 00 71 -14 7 E 1 7 6 14 2.5 42. 0.0 0.0 -0. 42. 7.5 10 51 1.4 92- 0 56 12 00 00 61 5E 0.1 6.8 0 01 61 06 00 01 81 -14 3 F 4 8 6 14 3.0 42. 0.0 0.0 -0. 42. 5.9 10 51 1.0 92- 0 39 12 00 00 40 8E 0.0 4.5 7 01 08 72 00 00 35 -14 7 G 8 4 6 14 3.8 42. 0.0 0.0 -0. 42. 6.0 10 51 1.0 92- 1 40 13 00 00 44 4E 0.1 5.0 6 01 16 29 00 01 97 -14 6 H 3 6 8 14 5.2 42. 0.0 0.0 -0. 42. 7.1 10 51 1.0 92- 0 43 12 00 00 52 8E 0.2 5.8 1 01I 29 90 00 03 20 -14 2 3 0 9 14 0.5 20. 0.0 0.0 0.1 -12 2.4 -61 -18 57. 92- 0 72 55 00 13 . 2E .9 9.8 22 02 66 14 00 57 83 -16 2 A 8 04 3 14 0.9 34. 0.0 0.3 0.0 24. 7.3 71. 31 10. 92- 0 85 18 90 33 90 9E 4 9.6 20 02 18 34 23 79 37 -15 5 B 2 9 14 1.3 42. 0.0 0.0 0.0 41. 8.2 97. 50 1.0 92- 0 81 13 00 03 65 5E 3 6.6 6 02 67 45 00 93 50 -14 5 C 9 6 14 1.6 42. 0.0 0.0 0.0 42. 1.6 99. 51 1.4 92- 0 49 12 00 00 38 3E 8 4.4 8 02 59 58 00 36 91 -13 1 D 1 2 14 2.2 42. 0.0 0.0 0.0 42. 1.5 99. 51 2.4 92- 1 39 12 00 00 30 3E 8 3.5 0 02 55 74 00 31 26 -13 0 E 2 7 14 2.9 42. 0.0 0.0 0.0 42. 2.0 99. 51 1.1 92- 0 44 13 00 00 36 9E 8 4.1 5 02 27 28 00 27 19 -13 3 F 7 3 14 4.0 42. 0.0 0.0 0.0 42. 2.5 99. 51 2.0 92- 1 38 12 00 00 34 7E 9 3.9 9 02 27 38 00 14 18 -13 2 G 1 6 14 5.2 42. 0.0 0.0 0.0 42. 8.1 99. 51 1.4 92- 0 54 12 19 00 42 8E 7 4.7 2 02 56 66 91 42 25 -14 7 H 1 5 14 0.5 25. 0.0 3.0 0.0 16. 1.7 66. 22 7.5 92- 0 22 26 15 29 72 2E 2 0.8 2 03 10 91 32 67 59 -15 0 A 9 3 14 0.9 44. 0.0 0.2 0.0 42. 3.1 94. 51 1.6 92- 0 43 14 76 07 14 8E 8 1.8 7 03 91 80 70 85 97 -14 9 B 2 0 14 1.3 43. 0.0 0.0 0.0 43. 7.9 99. 52 0.9 92- 0 62 12 00 01 30 6E 3 4.1 9 03 44 92 00 07 86 -14 0 C 2 4 14 1.6 43. 0.0 0.0 0.0 43. 6.3 99. 52 1.1 92- 0 48 13 17 00 27 0E 5 3.7 4 03 94 14 31 73 43 -14 4 D 0 1 14 2.2 43. 0.0 0.0 0.0 43. 1.0 99. 52 1.3 92- 1 32 13 06 00 21 6E 7 3.1 0 03 74 24 68 37 84 -13 5 E 1 6 14 2.9 43. 0.0 0.1 0.0 43. 1.1 99. 52 1.7 92- 0 38 12 04 00 20 1E 6 2.9 2 03 01 08 88 64 28 -13 9 F 2 3 14 4.0 43. 0.0 0.0 0.0 43. 1.5 99. 52 0.8 92- 1 28 13 46 00 23 9E 9 3.3 3 03 04 08 66 18 32 -13 1 G 7 6 14 5.1 43. 0.0 0.1 0.0 43. 1.5 99. 52 1.6 92- 9 38 12 17 00 24 8E 7 3.4 8 03 61 86 22 52 33 -13 1 H 0 2 HF bi- 14 0.3 40. -0. 0.0 -0. 49. 3.3 12 59 42. T3 otit 94- 0 51 04 00 03 80 8E 2.9 1.0 23 49 e 01 17 93 00 14 59 -16 8 A 4 7 8 5 14 0.6 48. 0.0 0.3 0.0 47. 1.1 97. 56 3.1 94- 0 51 13 13 03 52 2E 9 7.8 6 01 83 54 24 49 16 -14 1 B 8 3 14 0.9 47. 0.0 0.0 0.0 47. 5.3 99. 57 1.1 94- 0 95 12 00 00 87 0E 8 1.4 8 01 37 03 00 26 55 -14 3 C 2 5 14 1.2 48. 0.0 0.0 0.0 48. 6.9 10 57 1.5 94- 0 02 11 16 00 02 2E 0.0 2.9 4 01 67 97 02 02 13 -14 2 D 5 2 14 1.5 47. 0.0 0.0 0.0 47. 5.4 99. 56 1.4 94- 0 82 13 47 00 66 2E 7 9.2 4 01 36 15 06 55 50 -14 8 E 5 0 14 1.9 47. 0.0 0.0 -0. 47. 5.9 10 56 2.7 94- 0 64 11 24 00 65 3E 0.0 9.2 7 01 53 17 17 00 90 -14 2 F 0 4 6 14 2.4 47. 0.0 0.0 -0. 47. 6.2 10 57 1.2 94- 0 82 11 00 00 96 2E 0.3 2.3 3 01 91 31 00 04 06 -14 0 G 4 5 6 14 3.0 47. 0.0 0.0 -0. 47. 7.2 10 56 2.2 94- 0 60 10 00 00 62 1E 0.0 8.8 3 01 54 89 00 00 69 -14 9 H 8 7 5 14 3.8 47. 0.0 0.0 -0. 47. 1.1 10 57 1.3 94- 1 90 11 06 00 92 8E 0.0 1.9 6 01I 46 46 20 00 67 -13 6 4 7 2 14 5.1 48. 0.0 0.0 0.0 48. 1.5 99. 57 0.9 94- 9 10 12 11 00 05 5E 9 3.3 8 01 79 09 80 17 76 -13 0 J 8 4 14 0.6 47. 0.0 0.0 0.0 45. 1.1 96. 55 5.1 94- 0 44 12 00 04 98 9E 9 2.0 7 02 99 72 00 95 77 -14 2 A 7 7 14 1.0 48. 0.0 0.0 0.0 47. 4.9 99. 57 2.3 94- 0 36 13 27 01 92 9E 1 1.9 4 02 56 28 93 51 24 -14 1 B 6 0 14 1.4 47. 0.0 0.0 0.0 47. 6.0 99. 56 1.2 94- 0 87 12 00 00 70 3E 6 9.7 8 02 71 00 00 58 59 -14 0 C 6 6 14 1.9 47. 0.0 0.4 0.0 47. 8.4 99. 56 1.5 94- 0 76 11 10 00 66 0E 8 9.2 0 02 19 70 58 50 01 -14 3 D 9 3 14 2.5 48. 0.0 0.0 0.0 47. 8.9 99. 57 1.2 94- 0 00 12 00 00 94 9E 9 2.1 0 02 17 02 00 18 83 -14 8 E 2 0 14 3.0 47. 0.0 0.0 0.0 47. 7.2 99. 56 1.1 94- 1 73 11 00 00 59 3E 7 8.5 4 02 95 48 00 49 36 -14 5 F 5 3 14 3.7 47. 0.0 0.0 0.0 47. 1.1 99. 56 1.3 94- 1 72 12 06 00 54 1E 6 8.0 7 02 97 31 30 64 14 -13 1 G 6 7 14 4.4 47. 0.0 0.0 0.0 47. 1.0 99. 56 1.1 94- 1 73 11 00 00 70 5E 9 9.7 1 02 57 84 00 09 82 -13 2 H 8 7 14 5.1 47. 0.0 0.0 0.0 47. 4.6 99. 57 1.7 94- 8 99 12 05 00 88 3E 8 1.5 3 02I 85 63 17 38 58 -14 4 0 3 14 0.6 48. 0.0 0.2 0.0 43. 5.7 91. 52 5.1 94- 0 00 20 65 14 79 2E 2 9.2 0 03 60 96 00 34 84 -15 3 A 8 8 14 1.0 47. 0.0 0.0 0.0 47. 5.6 99. 56 1.7 94- 0 90 12 00 00 66 1E 5 9.2 6 03 41 52 00 81 39 -14 7 B 5 6 14 1.4 48. 0.0 0.0 0.0 48. 1.3 10 57 1.2 94- 0 01 11 00 00 01 5E 0.0 2.8 1 03 76 75 00 00 59 -13 7 C 7 5 14 1.9 48. 0.0 0.0 0.0 48. 8.9 99. 57 1.1 94- 0 15 11 08 00 08 3E 9 3.6 0 03 15 90 03 21 85 -14 1 D 3 5 14 2.5 47. 0.0 0.0 0.0 47. 8.6 10 57 1.2 94- 0 94 11 00 00 91 5E 0.0 1.8 1 03 08 05 00 07 90 -14 8 E 1 4 14 3.0 47. 0.0 0.0 0.0 47. 6.7 99. 57 1.3 94- 1 96 11 38 00 90 5E 9 1.7 5 03 73 78 09 23 40 -14 3 F 4 3 14 3.7 47. 0.0 0.0 -0. 47. 8.1 10 56 1.3 94- 1 61 10 00 00 72 1E 0.2 9.9 3 03 77 88 00 03 62 -14 1 G 3 7 0 14 4.4 47. 0.0 0.0 -0. 47. 1.0 10 57 1.1 94- 2 86 11 00 00 92 7E 0.1 1.9 9 03 19 70 00 02 42 -13 3 H 8 1 9 14 5.1 47. 0.0 0.0 0.0 47. 3.7 99. 56 1.5 94- 9 74 11 04 00 71 3E 9 9.8 6 03I 95 78 87 11 72 -13 1 6 3 HF bi- 14 0.4 40. 0.0 0.0 0.0 39. 3.5 96. 47 6.8 T3 otit 95- 0 45 13 00 04 04 0E 5 8.7 4 51 e 01 99 54 00 79 37 -15 4 A 2 0 14 0.8 47. 0.0 0.0 0.0 47. 3.7 99. 56 2.3 95- 0 59 12 00 00 38 7E 6 6.4 9 01 73 62 00 70 90 -14 5 B 5 2 14 1.2 47. 0.0 0.0 0.0 47. 2.5 99. 56 2.1 95- 0 54 14 00 01 22 7E 3 4.8 5 01 81 47 00 08 90 -14 1 C 2 6 14 1.6 46. 0.0 0.0 -0. 47. 1.9 10 56 4.3 95- 0 75 11 00 00 20 2E 1.0 4.5 6 01 27 65 00 15 17 -14 3 D 3 2 5 14 2.1 47. 0.0 0.0 0.0 47. 1.5 99. 56 2.2 95- 1 43 14 00 01 13 9E 4 3.8 9 01 70 10 00 02 51 -14 4 E 0 5 14 2.8 47. 0.0 0.0 -0. 47. 2.9 10 57 1.5 95- 0 69 14 00 00 77 5E 0.2 0.4 7 01 74 35 00 02 52 -14 1 F 1 6 2 14 3.5 47. 0.0 0.0 -0. 48. 8.3 10 57 3.1 95- 1 22 10 00 00 23 4E 2.1 5.0 2 01 35 77 00 34 34 -15 9 G 1 2 7 14 4.2 50. -0. 0.0 -0. 64. 7.6 12 73 21. 95- 1 83 01 00 04 46 4E 6.8 3.6 13 01 16 99 00 61 49 -16 3 H 7 4 5 5 14 5.1 46. 0.0 0.0 -0. 48. 1.2 10 57 12. 95- 9 65 08 00 00 26 9E 3.4 5.3 27 01I 64 53 00 54 08 -15 7 9 3 3 14 0.5 41. 0.0 0.1 0.0 36. 7.7 89. 45 3.6 95- 0 27 15 99 15 77 1E 1 4.0 9 02 70 82 61 32 05 -15 9 A 4 6 14 0.8 48. 0.0 0.1 0.0 47. 5.5 99. 56 1.5 95- 0 05 15 20 01 59 7E 0 8.5 3 02 34 10 60 61 13 -14 2 B 3 8 14 1.2 48. 0.0 0.0 0.0 48. 8.6 99. 57 1.4 95- 0 70 12 00 00 52 0E 6 8.0 3 02 58 81 00 63 02 -14 2 C 0 9 14 1.6 48. 0.0 0.0 0.0 48. 6.7 99. 57 1.4 95- 0 53 12 63 00 25 0E 4 5.3 3 02 56 34 34 96 77 -14 4 D 0 2 14 2.2 48. 0.0 0.0 0.0 48. 5.9 99. 57 1.1 95- 1 44 12 00 00 29 7E 7 5.7 5 02 69 93 00 52 28 -14 0 E 1 8 14 2.8 48. 0.0 0.0 0.0 48. 5.2 99. 57 1.3 95- 0 44 13 74 01 13 4E 4 4.1 2 02 94 88 18 08 95 -14 3 F 5 0 14 3.6 48. 0.0 0.0 0.0 48. 7.4 99. 57 1.4 95- 1 20 13 60 00 02 8E 6 2.9 5 02 70 45 38 63 60 -14 7 G 1 9 14 5.1 48. 0.0 0.0 0.0 48. 9.8 99. 57 2.0 95- 9 47 13 34 00 31 2E 7 5.9 8 02 95 18 99 55 96 -14 7 H 8 7 14 0.5 42. 0.0 0.6 0.0 35. 2.8 83. 43 9.0 95- 0 34 12 06 23 34 1E 4 8.4 9 03 62 40 68 89 69 -15 8 A 2 0 14 0.8 45. 0.0 0.1 0.0 45. 3.6 99. 54 1.6 95- 0 46 12 59 01 10 6E 2 2.8 4 03 93 46 43 29 40 -14 6 B 8 0 14 1.2 45. 0.0 0.0 0.0 45. 1.1 99. 54 1.1 95- 0 08 11 16 00 02 3E 9 2.0 7 03 97 20 17 21 95 -13 8 C 8 4 14 1.8 45. 0.0 0.0 0.0 45. 1.2 99. 54 1.4 95- 0 40 11 13 00 33 4E 8 5.2 7 03 85 57 53 25 52 -13 6 D 6 9 14 2.5 45. 0.0 0.0 0.0 44. 1.0 99. 54 1.0 95- 9 04 11 24 00 97 4E 9 1.5 0 03 29 78 01 22 99 -13 6 E 0 1 14 3.5 44. 0.0 0.0 0.0 44. 9.9 99. 54 1.6 95- 0 96 12 27 00 93 5E 9 1.1 4 03 54 41 55 11 65 -14 1 F 2 6 14 5.2 45. 0.0 0.0 0.0 45. 2.5 10 54 0.9 95- 0 30 11 00 00 28 6E 0.0 4.7 4 03 42 85 00 05 79 -13 7 G 4 3

H6 bi- 14 0.4 43. 0.0 0.0 0.0 38. 7.3 88. 47 3.8 81 otit 99- 0 14 14 00 16 28 9E 7 0.5 2 e 01 70 63 00 45 69 -15 7 A 9 6 14 0.8 43. 0.0 0.0 0.0 42. 1.0 99. 51 1.0 99- 0 04 12 00 00 85 6E 6 9.3 6 01 89 08 00 65 58 -13 4 B 2 3 14 1.2 43. 0.0 0.0 0.0 43. 7.0 99. 52 1.4 99- 0 17 11 00 00 14 1E 9 2.3 5 01 13 66 00 10 19 -14 5 C 8 1 14 2.6 43. 0.0 0.0 -0. 43. 1.6 10 52 1.1 99- 0 15 11 00 00 17 3E 0.0 2.6 9 01 60 64 00 00 43 -13 9 D 1 6 0 14 2.2 42. 0.0 0.0 -0. 43. 7.3 10 52 3.2 99- 1 63 10 00 00 49 5E 2.0 6.0 7 01 39 35 00 29 40 -15 4 E 3 1 4 14 2.8 42. 0.0 0.0 -0. 42. 9.6 10 51 3.0 99- 0 56 09 00 00 80 3E 0.5 8.7 6 01 93 26 00 07 04 -15 5 F 6 8 1 14 3.5 43. 0.0 0.0 -0. 43. 1.3 10 53 2.4 99- 1 59 10 00 00 90 6E 0.7 0.3 7 01 47 86 00 10 49 -14 5 G 4 5 1 14 4.2 44. 0.0 0.0 -0. 48. 2.0 10 57 11. 99- 1 99 05 00 01 22 0E 7.2 5.0 62 01 62 55 00 09 79 -15 4 H 5 4 3 14 5.1 43. 0.0 0.0 -0. 43. 2.4 10 52 1.9 99- 9 17 10 00 00 29 6E 0.3 3.9 4 01I 01 60 00 04 87 -14 9 4 4 1 H6 bi- 14 0.5 48. 0.0 0.2 0.0 34. 1.2 70. 42 4.3 81 otit 99- 0 33 19 39 48 05 6E 4 4.2 5 e 02 96 49 87 42 53 -14 0 A 9 5 14 0.8 44. 0.0 0.0 0.0 43. 1.0 97. 52 1.3 99- 0 39 11 00 04 11 7E 1 2.0 5 02 08 18 00 32 42 -13 6 B 8 5 14 1.2 43. 0.0 0.0 0.0 43. 1.9 99. 52 1.5 99- 0 26 12 00 00 23 6E 9 3.2 6 02 42 37 00 11 17 -13 9 C 3 5 14 1.7 43. 0.0 0.0 0.0 43. 1.7 99. 52 1.2 99- 0 29 12 00 00 25 7E 9 3.5 7 02 80 03 00 14 67 -13 5 D 5 7 14 2.5 43. 0.0 0.0 0.0 43. 2.9 99. 52 1.1 99- 0 21 11 00 00 18 0E 9 2.8 9 02 45 97 00 09 85 -13 4 E 2 8 14 3.4 42. 0.0 0.0 0.0 42. 1.6 99. 51 1.1 99- 1 89 11 00 00 87 7E 9 9.5 8 02 82 67 00 09 23 -13 1 F 4 3 14 4.3 43. 0.0 0.0 -0. 43. 8.9 10 52 1.2 99- 1 17 11 00 00 25 7E 0.2 3.5 5 02 35 47 00 02 53 -14 4 G 2 8 7 14 5.1 42. 0.0 0.0 0.0 42. 4.4 99. 51 1.5 99- 9 86 11 59 00 83 4E 9 9.1 2 02 72 63 95 12 90 -14 6 H 6 1 14 0.5 43. 0.0 0.3 0.0 39. 2.1 90. 48 2.4 99- 0 62 16 59 13 55 2E 7 4.2 9 03 13 27 81 89 53 -14 4 A 0 7 14 0.8 42. 0.0 0.0 0.0 42. 1.1 99. 51 1.4 99- 0 93 13 28 00 67 2E 4 7.3 9 03 10 48 01 89 12 -13 9 B 2 7 14 1.2 42. 0.0 0.0 0.0 42. 1.0 99. 51 1.4 99- 0 76 12 00 00 74 4E 9 8.1 8 03 54 47 00 08 17 -13 3 C 8 8 14 1.7 42. 0.0 0.0 0.0 42. 1.4 99. 52 1.0 99- 0 99 12 00 00 93 0E 8 0.1 2 03 83 01 00 22 25 -13 4 D 8 8 14 2.5 42. 0.0 0.0 0.0 42. 1.4 99. 51 1.0 99- 0 85 12 00 00 78 3E 8 8.6 8 03 55 52 00 24 55 -13 0 E 8 6 14 3.6 42. 0.0 0.0 -0. 42. 5.6 10 51 1.2 99- 1 66 12 00 00 67 5E 0.0 7.4 7 03 75 27 00 00 17 -14 0 F 9 2 2 14 5.1 42. 0.0 0.0 0.0 42. 4.0 99. 51 1.7 99- 8 58 11 36 00 53 5E 9 6.0 6 03 52 92 95 17 91 -14 0 G 5 0 H6 bi- 15 0.4 44. 0.0 0.0 -0. 44. 1.0 10 53 2.6 87 otit 01- 0 49 08 00 00 73 4E 0.5 8.9 5 B e 01 78 44 00 08 27 -14 9 A 1 0 7 15 0.7 45. 0.0 0.0 -0. 46. 2.2 10 55 2.9 01- 0 83 10 00 00 07 2E 0.5 2.8 7 01 53 17 00 08 19 -14 9 B 3 0 8 15 1.1 46. 0.0 0.0 0.0 46. 2.1 99. 55 1.7 01- 1 49 10 37 00 46 6E 9 6.9 0 01 44 41 34 11 61 -14 6 C 3 9 15 1.6 46. 0.0 0.0 -0. 46. 1.2 10 55 2.7 01- 0 49 09 00 00 66 5E 0.4 9.0 2 01 45 39 00 05 38 -14 0 D 4 8 9 15 2.1 45. 0.0 0.8 0.0 44. 6.5 99. 53 6.3 01- 1 11 09 70 01 67 2E 0 8.3 9 01 71 33 39 83 01 -15 4 E 7 2 15 2.8 43. 0.0 3.0 0.0 43. 4.0 99. 52 5.3 01- 0 98 12 68 02 68 4E 1 8.0 0 01 16 08 66 12 30 -15 3 F 5 9 15 3.6 43. -0. 0.0 -0. 46. 1.3 10 55 16. 01- 1 75 00 00 00 09 0E 5.4 3.1 43 01 22 69 00 79 48 -15 2 G 5 5 4 2 15 5.2 44. 0.0 0.1 -0. 45. 6.8 10 55 5.5 01- 0 77 05 81 00 97 8E 2.7 1.8 2 01 83 69 91 39 47 -15 8 H 7 9 2 15 0.4 49. 0.0 0.3 0.0 42. 1.3 85. 51 2.7 01- 0 77 14 02 23 74 6E 9 8.2 5 02 64 96 04 89 91 -14 1 A 4 4 15 0.7 44. 0.0 0.0 0.0 43. 3.4 98. 52 1.2 01- 0 27 12 62 02 55 5E 4 6.6 1 02 23 44 68 45 43 -14 8 B 5 7 15 1.1 44. 0.0 0.0 0.0 43. 3.3 99. 52 1.2 01- 0 10 12 70 01 65 8E 0 7.7 1 02 37 64 02 54 53 -14 3 C 9 0 15 1.6 44. 0.0 0.1 0.0 43. 2.8 99. 53 1.6 01- 0 16 11 68 00 95 7E 5 0.8 4 02 21 11 36 76 40 -14 6 D 0 5 15 2.4 43. 0.0 0.2 0.0 43. 2.4 99. 52 1.4 01- 0 73 12 34 01 40 5E 2 5.1 8 02 46 49 77 19 81 -14 4 E 9 6 15 3.6 43. 0.0 0.0 0.0 43. 1.4 99. 52 1.8 01- 1 48 11 89 00 45 3E 9 5.6 7 02 66 11 04 13 77 -14 6 F 8 9 15 5.2 43. 0.0 0.0 -0. 43. 1.2 10 52 2.2 01- 0 58 11 00 00 59 8E 0.0 7.0 5 02 04 01 00 00 28 -14 8 G 3 4 1 15 0.4 49. 0.0 0.6 0.0 40. 9.2 81. 49 3.5 01- 0 71 15 64 30 68 1E 8 6.2 0 03 54 62 45 81 08 -15 9 A 6 3 15 0.7 45. 0.0 0.0 0.0 44. 4.4 98. 53 1.5 01- 0 54 12 00 03 65 3E 0 8.1 0 03 45 04 00 01 43 -14 8 B 4 2 15 1.1 44. 0.0 0.0 0.0 44. 5.2 99. 53 1.1 01- 0 96 11 51 00 78 5E 6 9.4 5 03 01 58 74 62 09 -14 9 C 6 4 15 1.6 44. 0.0 0.0 -0. 45. 4.5 10 54 1.2 01- 0 99 10 00 00 08 3E 0.2 2.6 5 03 72 73 00 02 02 -14 1 D 7 8 1 15 2.4 44. 0.0 0.0 -0. 44. 3.8 10 54 1.3 01- 0 75 10 00 00 83 2E 0.2 0.1 7 03 01 06 00 03 88 -14 0 E 8 0 4 15 3.6 44. 0.0 0.0 -0. 45. 1.9 10 54 1.6 01- 1 80 10 00 00 16 5E 0.8 3.4 4 03 57 00 00 12 09 -14 5 F 5 0 6 15 5.1 45. 0.0 0.4 0.0 44. 1.8 99. 54 2.4 01- 9 16 11 11 00 96 7E 5 1.4 8 03 22 49 18 81 65 -14 3 G 9 3 H6 mu 15 0.5 32. 0.1 22. 0.1 -7. 3.2 -22 -10 56. 87 sco 02- 0 71 11 51 42 57 5E .8 9.6 49 B vit 01 00 97 63 05 22 -16 0 e A 7 7 7 15 0.9 43. 0.0 0.0 0.0 39. 2.6 91. 48 7.9 02- 0 06 09 00 12 42 1E 5 2.8 3 01 99 68 00 32 69 -15 6 B 0 6 15 1.4 44. 0.0 0.0 0.0 43. 8.5 98. 52 1.0 02- 0 34 11 00 01 83 0E 8 9.6 7 01 91 74 00 74 33 -14 0 C 6 4 15 1.9 43. 0.0 0.0 0.0 43. 3.6 99. 52 1.0 02- 0 71 11 13 00 66 8E 9 7.8 8 01 20 56 38 17 15 -13 0 D 9 1 15 2.3 43. 0.0 0.0 -0. 43. 8.9 10 52 1.2 02- 1 61 11 00 00 63 2E 0.1 7.5 9 01 04 56 00 00 62 -14 3 E 3 9 2 15 2.7 43. 0.0 0.0 -0. 43. 2.7 10 52 1.8 02- 0 34 11 00 00 47 3E 0.3 5.8 0 01 57 19 00 04 06 -14 0 F 5 2 0 15 3.7 43. 0.0 0.0 -0. 43. 2.5 10 53 1.6 02- 1 87 11 00 00 95 7E 0.2 0.8 0 01 05 55 00 02 58 -14 8 G 6 9 0 15 5.1 44. 0.0 0.0 -0. 44. 9.6 10 53 1.1 02- 9 34 11 00 00 39 3E 0.1 5.4 6 01 39 39 00 01 58 -14 8 H 3 8 9 15 0.8 44. 0.0 15. 0.0 27. 8.1 62. 35 19. 02- 0 01 62 20 59 83 3E 6 3.8 14 02 54 70 63 78 55 -16 1 A 2 7 0 15 1.2 53. 0.0 2.2 0.0 44. 4.0 83. 53 6.0 02- 0 01 19 86 31 06 1E 0 2.0 3 02 74 38 92 12 77 -15 5 B 5 9 15 1.6 45. 0.0 0.0 0.0 44. 1.5 99. 54 0.9 02- 0 11 12 48 00 85 4E 4 0.2 9 02 84 03 07 92 00 -13 1 C 5 6 15 1.8 44. 0.0 0.0 0.0 44. 1.6 10 53 1.5 02- 0 51 11 17 00 50 1E 0.0 6.6 0 02 85 73 91 06 29 -13 0 D 2 3 15 2.2 44. 0.0 0.0 0.0 44. 3.4 99. 53 2.2 02- 1 61 11 50 00 55 7E 9 7.1 2 02 02 35 36 20 62 -14 5 E 0 7 15 3.7 44. 0.0 1.1 0.0 44. 2.4 99. 53 1.7 02- 1 20 11 90 00 07 3E 6 2.1 7 02 67 83 72 87 86 -14 7 F 2 3 15 5.2 44. 0.0 0.0 -0. 44. 4.0 10 53 1.2 02- 0 21 10 29 00 30 9E 0.2 4.5 1 02 50 56 90 03 51 -14 3 G 0 0 3 15 0.8 41. -0. 0.0 -0. 46. 1.0 11 55 13. 02- 0 78 01 00 01 55 1E 1.4 7.8 47 03 77 14 00 61 42 -15 7 A 3 4 4 4 15 1.2 45. 0.0 0.0 0.0 44. 4.8 98. 53 4.6 02- 0 21 12 00 03 32 0E 0 4.7 1 03 87 24 00 03 40 -15 3 B 6 0 15 1.6 44. 0.0 0.0 0.0 44. 1.5 99. 53 0.9 02- 0 39 11 00 00 24 9E 7 3.9 3 03 12 73 00 48 82 -13 4 C 9 8 15 1.8 44. 0.0 0.0 -0. 44. 1.8 10 53 1.2 02- 0 26 11 00 00 30 1E 0.1 4.5 6 03 93 19 00 01 76 -13 6 D 4 3 1 15 2.2 44. 0.0 0.0 -0. 44. 5.7 10 53 1.7 02- 1 17 11 00 00 30 7E 0.3 4.5 2 03 46 06 00 04 31 -14 1 E 6 4 6 15 3.7 44. 0.0 0.0 -0. 44. 4.4 10 53 1.7 02- 1 04 10 00 00 25 4E 0.5 3.9 5 03 88 71 00 06 08 -14 7 F 1 9 0 15 5.1 44. 0.0 0.0 -0. 44. 4.2 10 53 1.8 02- 9 33 10 00 00 56 4E 0.5 7.2 4 03 68 56 00 07 47 -14 4 G 7 7 0 H6 bi- 15 0.4 42. 0.0 0.0 -0. 43. 3.0 10 52 6.0 90 otit 03- 0 70 04 00 00 56 9E 2.0 6.7 3 e 01 67 98 00 28 00 -15 4 A 1 9 1 15 0.7 43. 0.0 0.0 -0. 44. 2.7 10 53 1.2 03- 0 59 10 00 00 01 4E 1.0 1.4 7 01 36 06 00 14 11 -14 6 B 1 2 4 15 1.1 44. 0.0 0.0 -0. 44. 6.9 10 53 1.2 03- 1 02 10 00 00 11 3E 0.2 2.5 4 01 70 81 00 03 46 -14 4 C 5 0 8 15 1.5 44. 0.0 0.0 -0. 44. 7.3 10 53 1.2 03- 0 17 11 00 00 27 7E 0.2 4.2 3 01 12 04 00 03 73 -14 4 D 4 6 4 15 1.9 44. 0.0 0.0 -0. 44. 7.4 10 53 1.0 03- 0 43 11 00 00 50 3E 0.2 6.6 5 01 25 40 00 02 46 -14 2 E 6 5 8 15 2.3 44. 0.0 0.0 -0. 44. 6.1 10 53 1.0 03- 1 26 11 00 00 33 6E 0.2 4.8 1 01 48 29 00 02 78 -14 7 F 5 5 0 15 2.8 43. 0.0 0.0 -0. 44. 4.1 10 53 1.7 03- 0 95 11 00 00 07 8E 0.3 2.1 1 01 95 09 00 04 73 -14 5 G 9 0 6 15 3.7 44. 0.0 0.0 0.0 44. 2.9 99. 53 1.4 03- 1 37 12 05 00 19 6E 6 3.3 3 01 99 66 60 63 32 -14 6 H 6 6 15 5.2 44. 0.0 0.4 0.0 44. 2.1 99. 53 1.7 03- 0 50 11 33 00 36 9E 7 5.2 8 01I 37 66 72 61 88 -14 0 7 5 15 0.5 46. 0.0 0.0 0.0 44. 1.1 94. 53 2.8 03- 0 98 13 15 08 57 1E 9 7.3 3 02 30 59 18 14 83 -14 8 A 4 2 15 0.8 45. 0.0 0.0 0.0 45. 4.5 99. 54 1.0 03- 0 19 11 00 00 15 9E 9 3.4 5 02 05 66 00 11 82 -14 2 B 2 7 15 1.2 45. 0.0 0.0 0.0 45. 5.7 10 54 1.3 03- 0 55 11 65 00 55 3E 0.0 7.5 4 02 34 14 79 01 59 -14 5 C 9 9 15 1.5 45. 0.0 0.0 0.0 45. 3.9 10 54 1.6 03- 0 58 11 45 00 58 0E 0.0 7.8 5 02 48 05 25 02 44 -14 4 D 1 0 15 1.9 45. 0.0 0.3 0.0 45. 4.7 99. 54 2.7 03- 0 61 11 12 00 39 4E 5 5.9 5 02 21 99 21 84 79 -14 1 E 0 6 15 2.3 45. 0.0 0.2 0.0 45. 4.0 99. 54 1.3 03- 1 58 12 32 00 49 3E 8 6.8 5 02 17 27 74 38 28 -14 9 F 4 6 15 3.5 45. 0.0 0.4 0.0 45. 5.3 99. 54 1.2 03- 0 51 11 33 00 35 7E 6 5.4 9 02 62 69 99 71 18 -14 3 G 0 8 15 5.2 45. 0.0 0.4 0.0 45. 2.6 99. 54 2.0 03- 0 91 12 53 01 59 2E 3 7.9 5 02 01 85 91 24 36 -14 4 H 0 8 15 0.5 43. 0.0 1.3 0.0 41. 3.8 95. 50 5.8 03- 0 63 16 00 07 55 4E 2 5.5 4 03 48 24 01 50 55 -15 9 A 4 2 15 0.8 44. 0.0 0.8 0.0 44. 1.2 97. 53 2.1 03- 0 96 12 38 03 05 4E 9 1.9 9 03 60 94 86 39 38 -14 1 B 3 3 15 1.2 45. 0.0 0.0 -0. 45. 2.8 10 54 1.6 03- 0 19 11 00 00 21 5E 0.1 4.0 2 03 15 33 00 00 89 -14 5 C 4 9 5 15 1.5 44. 0.0 0.0 -0. 45. 4.4 10 54 1.2 03- 0 96 11 00 00 02 0E 0.1 2.0 6 03 49 18 00 02 91 -14 8 D 5 2 1 15 1.9 45. 0.0 0.0 -0. 45. 2.8 10 54 1.6 03- 0 41 10 00 00 56 8E 0.3 7.6 8 03 82 65 00 05 85 -14 8 E 9 1 3 15 2.3 45. 0.0 0.0 -0. 45. 3.0 10 54 1.6 03- 1 11 10 00 00 31 1E 0.4 5.0 2 03 73 38 00 06 21 -14 2 F 4 6 9 15 3.5 45. 0.0 0.0 -0. 45. 3.9 10 54 1.4 03- 0 13 10 00 00 28 3E 0.3 4.7 5 03 08 69 00 05 64 -14 5 G 6 3 9 15 5.1 44. 0.0 0.1 0.0 44. 2.2 99. 53 1.6 03- 9 93 11 78 00 76 4E 6 9.3 1 03 17 47 75 62 68 -14 5 H 0 9 SP A0 10 4-4 6 HF bi- 15 0.4 39. 0.0 0.0 -0. 39. 3.0 10 46 5.4 T3 otit 06- 0 21 12 00 00 57 3E 0.9 3.4 1 53 e 01 00 82 00 12 54 -15 1 B A 3 4 1 15 0.7 46. 0.0 0.0 0.0 46. 5.4 99. 53 1.0 06- 0 98 16 00 00 81 7E 6 6.6 7 01 20 40 00 58 06 -14 2 B 9 1 15 1.1 46. 0.0 0.0 0.0 46. 7.3 99. 53 1.0 06- 0 90 17 00 00 87 1E 9 7.2 6 01 09 06 00 09 55 -14 6 C 9 3 15 1.6 47. 0.0 0.0 0.0 46. 5.4 99. 53 1.5 06- 0 14 17 70 00 93 3E 5 7.8 9 01 79 41 29 75 43 -14 4 D 5 3 15 2.2 46. 0.0 0.0 0.0 46. 6.2 99. 53 1.5 06- 1 54 17 00 00 46 0E 8 3.2 9 01 79 12 00 28 64 -14 0 E 2 8 15 2.8 46. 0.0 0.0 0.0 46. 6.2 99. 53 1.0 06- 0 84 17 00 00 80 5E 9 6.5 6 01 63 22 00 14 40 -14 5 F 7 5 15 3.7 46. 0.0 0.0 -0. 46. 4.6 10 53 1.3 06- 1 77 17 00 00 78 4E 0.0 6.3 7 01 35 54 00 00 70 -14 8 G 3 4 0 15 5.2 46. 0.0 0.2 0.0 45. 8.4 98. 52 3.6 06- 0 44 18 24 02 76 9E 5 6.1 2 01 69 87 56 41 10 -15 8 H 5 8 15 0.5 45. 0.0 0.8 0.0 43. 9.5 95. 49 2.9 06- 0 12 21 48 07 03 0E 3 8.7 3 02 54 44 75 39 38 -15 7 A 8 5 15 0.8 46. 0.0 0.1 0.0 46. 2.9 99. 53 1.7 06- 0 96 15 24 01 49 4E 0 3.4 0 02 30 09 83 63 58 -14 9 B 5 2 15 1.2 46. 0.0 0.0 -0. 46. 2.9 10 53 1.5 06- 0 81 14 00 00 90 5E 0.2 7.5 3 02 93 17 00 03 74 -14 8 C 9 0 3 15 1.8 46. 0.0 0.2 0.0 46. 3.5 99. 53 1.3 06- 0 51 14 20 00 37 6E 7 2.2 1 02 52 15 12 57 06 -14 5 D 3 4 15 2.5 46. 0.0 0.0 -0. 46. 3.7 10 53 1.5 06- 0 67 13 00 00 73 5E 0.1 5.9 3 02 09 50 00 02 79 -14 0 E 7 3 9 15 3.4 46. 0.0 0.0 -0. 46. 3.8 10 53 1.1 06- 1 54 12 00 00 64 9E 0.2 4.9 2 02 53 90 00 03 12 -14 4 F 1 3 4 15 5.2 46. 0.0 0.0 -0. 46. 4.1 10 53 1.0 06- 0 67 13 00 00 78 9E 0.2 6.3 5 02 37 38 00 03 17 -14 3 G 3 7 1 15 0.5 45. 0.0 0.9 0.0 40. 7.8 89. 47 2.9 06- 0 65 18 16 16 97 5E 7 7.8 5 03 42 60 06 16 61 -15 2 A 7 5 15 0.8 47. 0.0 0.1 0.0 46. 3.4 99. 53 1.3 06- 0 25 15 31 01 95 2E 4 8.0 1 03 20 41 80 05 55 -14 5 B 1 8 15 1.2 47. 0.0 0.0 0.0 47. 4.5 10 54 1.1 06- 0 35 15 00 00 33 3E 0.0 1.8 0 03 61 70 00 08 38 -14 0 C 8 5 15 1.7 46. 0.0 0.0 -0. 47. 3.7 10 53 1.1 06- 0 99 15 00 00 03 1E 0.1 8.8 9 03 25 42 00 01 34 -14 3 D 3 4 9 15 2.3 47. 0.0 0.0 -0. 47. 2.9 10 54 2.0 06- 1 07 14 00 00 20 6E 0.3 0.5 3 03 90 94 00 04 40 -14 1 E 3 2 0 15 3.0 46. 0.0 0.0 -0. 46. 2.9 10 53 1.4 06- 0 74 15 00 00 94 8E 0.4 7.9 6 03 65 47 00 06 95 -14 9 F 1 9 5 15 5.1 47. 0.0 0.0 -0. 47. 5.2 10 54 1.7 06- 9 07 15 00 00 16 3E 0.2 0.1 7 03 61 26 00 03 47 -14 3 G 8 0 1 HF bi- 15 0.4 47. 0.0 0.0 0.0 43. 7.8 92. 50 3.8 T3 otit 07- 0 40 13 00 12 68 6E 1 5.3 0 55 e 01 62 01 00 61 05 -15 1 A 2 9 15 0.7 52. 0.0 0.1 0.0 51. 3.6 98. 58 1.4 07- 0 50 13 38 03 62 0E 3 3.7 4 01 30 44 86 04 11 -14 0 B 1 2 15 1.1 53. 0.0 0.0 0.0 53. 6.2 99. 59 1.3 07- 0 16 12 00 00 09 8E 9 7.9 3 01 15 71 00 22 68 -14 0 C 6 7 15 1.5 53. 0.0 0.0 0.0 53. 5.0 99. 59 1.3 07- 0 05 12 80 00 02 2E 9 7.2 3 01 35 66 83 12 55 -14 1 D 2 4 15 1.9 53. 0.0 0.3 0.0 52. 3.1 99. 59 1.5 07- 0 35 13 11 01 99 8E 3 6.9 4 01 11 63 80 31 94 -14 6 E 2 4 15 2.5 53. 0.0 0.0 0.0 52. 3.8 99. 59 1.3 07- 0 02 12 00 00 94 4E 9 6.4 5 01 63 13 00 26 93 -14 8 F 3 8 15 3.7 52. 0.0 0.0 0.0 52. 6.8 99. 59 1.3 07- 1 99 13 08 00 88 3E 8 5.8 3 01 85 42 63 38 62 -14 8 G 3 4 15 5.2 52. 0.0 0.0 0.0 52. 2.0 99. 59 2.0 07- 0 88 12 00 00 62 7E 5 3.3 0 01 41 65 00 87 54 -14 7 H 5 0 HF bi- 15 0.5 29. 0.0 0.0 0.0 27. 6.4 92. 33 2.2 T3 otit 07- 0 32 15 05 07 25 7E 9 1.4 7 55 e 02 81 17 23 02 39 -15 6 A 9 8 15 0.8 50. 0.0 0.0 -0. 50. 4.4 10 56 1.4 07- 0 06 13 00 00 09 0E 0.1 8.8 8 02 05 32 00 01 03 -14 5 B 5 0 9 15 1.2 52. 0.0 0.0 -0. 52. 7.7 10 59 1.1 07- 0 58 13 00 00 63 9E 0.1 3.4 3 02 03 68 00 01 66 -14 8 C 8 9 4 15 1.5 53. 0.0 0.0 -0. 53. 5.3 10 60 1.3 07- 0 33 13 00 00 43 7E 0.2 1.1 8 02 43 58 00 03 91 -14 8 D 8 6 7 15 2.0 53. 0.0 0.0 -0. 53. 6.0 10 59 1.4 07- 1 14 13 00 00 18 8E 0.1 8.7 3 02 08 05 00 01 06 -14 0 E 0 4 3 15 2.7 52. 0.0 0.0 -0. 53. 5.6 10 59 1.2 07- 0 94 13 00 00 04 1E 0.2 7.3 0 02 84 54 00 03 23 -14 8 F 1 2 3 15 3.5 52. 0.0 0.0 -0. 53. 6.7 10 59 1.7 07- 0 84 13 00 00 04 7E 0.4 7.3 5 02 82 14 00 06 32 -14 8 G 4 6 7 15 5.2 53. 0.0 0.0 -0. 53. 7.4 10 59 1.2 07- 0 02 13 00 00 15 9E 0.2 8.4 1 02 24 46 00 04 42 -14 5 H 0 5 3 15 0.5 38. 0.0 0.0 0.0 37. 9.6 98. 44 2.2 07- 0 08 11 00 01 51 3E 5 1.9 1 03 11 88 00 92 18 -15 7 A 0 3 15 0.8 51. 0.0 0.0 0.0 51. 4.1 10 58 1.5 07- 0 27 14 00 00 25 2E 0.0 0.1 8 03 34 10 00 06 66 -14 7 B 5 0 15 1.2 52. 0.0 0.0 -0. 52. 5.8 10 59 1.4 07- 0 79 13 00 00 94 0E 0.3 6.4 5 03 12 23 00 05 73 -14 6 C 8 3 1 15 1.6 53. 0.0 0.0 -0. 53. 4.3 10 59 2.0 07- 0 13 13 00 00 28 4E 0.3 9.6 6 03 28 29 00 05 05 -14 6 D 2 0 8 15 2.2 53. 0.0 0.0 -0. 53. 4.5 10 59 1.4 07- 1 07 13 00 00 11 2E 0.1 8.1 6 03 65 64 00 01 91 -14 1 E 8 4 9 15 3.0 52. 0.0 0.0 -0. 52. 5.6 10 59 1.5 07- 1 68 13 00 00 68 3E 0.0 3.9 9 03 21 65 00 00 92 -14 9 F 7 2 9 15 5.1 52. 0.0 0.0 -0. 52. 8.2 10 59 1.6 07- 9 33 13 00 00 36 1E 0.1 0.9 0 03 94 88 00 01 95 -14 1 G 2 0 4 HF mu 15 0.5 47. 0.0 3.0 0.0 39. 1.7 84. 46 10. T3 sco 09- 0 11 27 02 25 94 8E 6 7.1 46 56 vit 01 23 47 17 34 06 -15 8 e A 9 8 15 0.9 49. 0.0 0.3 0.0 49. 2.8 99. 56 1.6 09- 0 86 12 56 01 40 0E 1 2.1 4 01 70 20 55 69 66 -14 8 B 9 4 15 1.4 50. 0.0 0.0 0.0 50. 1.1 99. 56 1.2 09- 0 17 11 00 00 08 8E 8 8.7 9 01 72 91 00 31 37 -13 9 C 6 9 15 1.9 49. 0.0 0.0 0.0 49. 6.0 99. 56 1.2 09- 0 80 11 88 00 77 4E 9 5.7 3 01 82 61 19 15 24 -14 5 D 2 0 15 2.5 50. 0.0 0.9 0.0 50. 1.0 99. 56 3.2 09- 0 11 11 14 00 09 4E 9 8.8 8 01 16 97 45 41 21 -14 7 E 4 6 15 3.2 49. 0.0 0.7 0.0 49. 7.0 10 56 2.7 09- 0 83 13 74 00 87 6E 0.0 6.7 2 01 17 35 43 13 85 -15 9 F 5 3 15 4.5 48. 0.0 3.5 0.0 49. 3.3 10 55 8.3 09- 1 98 22 93 01 09 9E 0.0 9.0 0 01 74 15 70 00 12 -15 9 G 7 4 15 5.1 50. 0.0 0.4 0.0 49. 1.4 99. 56 2.4 09- 9 03 11 73 00 94 6E 8 7.4 8 01 78 69 02 48 69 -14 5 H 1 1 15 0.6 45. 0.0 0.0 0.0 42. 7.4 92. 49 3.7 09- 0 93 15 00 11 56 2E 7 4.0 8 02 54 82 00 41 45 -15 2 A 5 4 15 1.0 49. 0.0 0.0 0.0 49. 4.2 99. 56 1.4 09- 0 97 11 71 00 93 2E 9 7.3 1 02 16 90 26 13 95 -14 8 B 9 7 15 1.2 49. 0.0 0.1 0.0 49. 6.2 99. 56 1.1 09- 0 70 12 26 00 62 8E 8 4.3 8 02 05 37 66 31 35 -14 0 C 9 0 15 1.4 49. 0.0 0.0 -0. 49. 4.6 10 56 1.5 09- 0 44 11 00 00 55 4E 0.2 3.6 5 02 47 83 00 03 82 -14 6 D 5 9 5 15 1.9 49. 0.0 0.0 0.0 49. 5.3 99. 56 2.7 09- 0 59 12 51 00 48 3E 8 2.9 0 02 95 43 35 41 25 -14 2 E 6 2 15 3.8 50. 0.0 0.0 -0. 50. 3.6 10 56 2.0 09- 1 06 11 00 00 18 7E 0.3 9.8 8 02 29 36 00 04 99 -14 2 F 5 3 3 15 5.1 49. 0.0 0.0 -0. 49. 2.9 10 56 1.5 09- 9 73 12 00 00 89 4E 0.3 6.9 4 02 69 10 00 05 85 -14 8 G 9 5 3 15 0.6 40. 0.0 0.0 -0. 41. 4.8 10 48 3.8 09- 0 55 09 00 00 21 9E 1.6 0.2 2 03 60 10 00 22 45 -15 6 A 8 3 0 15 1.0 50. 0.0 0.0 -0. 50. 3.3 10 57 1.9 09- 0 41 09 00 00 55 7E 0.3 3.3 1 03 16 89 00 04 57 -14 8 B 8 9 6 15 1.2 49. 0.0 0.0 -0. 50. 4.9 10 56 2.0 09- 0 82 10 00 00 04 0E 0.4 8.4 7 03 85 78 00 07 47 -14 1 C 8 3 6 15 1.4 49. 0.0 0.0 -0. 49. 2.4 10 56 1.4 09- 0 71 10 00 00 93 4E 0.4 7.3 6 03 46 75 00 07 71 -14 6 D 3 6 5 15 1.9 49. 0.0 0.0 0.0 49. 8.6 10 56 1.1 09- 0 72 12 00 00 72 6E 0.0 5.2 4 03 87 05 00 02 15 -14 5 E 1 0 15 3.8 49. 0.0 0.0 -0. 49. 3.2 10 56 1.6 09- 1 84 11 00 00 87 1E 0.1 6.7 4 03 81 27 00 01 78 -14 8 F 4 0 7 15 5.2 50. 0.0 0.0 -0. 50. 1.3 10 56 2.6 09- 0 07 11 00 00 12 5E 0.1 9.2 7 03 79 19 00 01 99 -14 4 G 3 8 7 HF bi- 15 0.4 40. 0.0 2.3 0.0 37. 3.2 91. 44 5.4 T3 otit 10- 0 80 15 78 11 53 4E 9 2.2 8 58 e 01 37 38 10 88 79 -15 5 A 5 4 15 0.7 50. 0.0 0.3 0.0 50. 1.9 99. 56 1.9 10- 0 37 13 59 01 03 2E 3 8.2 6 01 87 26 88 31 10 -14 7 B 0 2 15 1.1 50. 0.0 0.1 0.0 50. 4.2 99. 56 1.5 10- 0 27 13 94 00 01 6E 5 8.1 6 01 13 18 72 94 53 -14 2 C 7 1 15 1.5 50. 0.0 0.0 0.0 50. 4.5 99. 56 1.1 10- 0 11 12 20 00 09 4E 9 8.8 8 01 75 73 23 10 00 -14 5 D 3 4 15 2.0 50. 0.0 0.3 0.0 50. 4.6 99. 56 1.4 10- 1 20 13 71 00 17 7E 9 9.6 9 01 94 25 91 25 57 -14 8 E 4 3 15 2.6 49. 0.0 0.1 0.0 49. 5.4 10 56 1.2 10- 0 90 12 41 00 90 1E 0.0 7.0 2 01 46 68 00 06 19 -14 1 F 9 2 15 3.7 50. 0.0 0.0 0.0 49. 9.4 99. 56 1.0 10- 1 00 12 60 00 98 7E 9 7.8 1 01 98 77 99 10 58 -14 3 G 2 5 15 5.1 49. 0.0 0.1 -0. 49. 7.6 10 56 1.1 10- 9 90 12 53 00 93 7E 0.1 7.3 1 01 04 28 77 00 35 -14 2 H 6 6 9 15 0.5 44. 0.0 0.0 0.0 44. 3.7 99. 51 4.7 10- 0 70 05 00 00 55 3E 7 4.1 2 02 60 96 00 49 89 -15 5 A 3 3 15 0.8 49. 0.0 0.0 0.0 49. 2.2 99. 56 1.5 10- 0 95 12 00 01 57 9E 2 3.8 9 02 34 77 00 28 36 -14 1 B 0 9 15 1.2 50. 0.0 0.0 -0. 50. 4.0 10 56 1.6 10- 0 04 12 00 00 11 6E 0.2 9.1 6 02 19 42 00 02 94 -14 3 C 6 6 2 15 1.6 49. 0.0 0.0 0.0 49. 5.0 99. 56 1.3 10- 0 81 13 00 00 78 9E 9 5.8 9 02 15 02 00 09 34 -14 6 D 2 2 15 2.2 50. 0.0 0.0 -0. 50. 4.6 10 56 1.3 10- 1 11 12 00 00 17 7E 0.1 9.6 9 02 61 53 00 02 69 -14 9 E 4 1 0 15 2.9 50. 0.0 0.2 0.0 49. 3.6 99. 56 1.7 10- 0 04 13 61 00 87 1E 6 6.7 2 02 41 36 69 67 44 -14 5 F 4 6 15 3.7 50. 0.0 0.0 0.0 50. 3.7 99. 56 1.5 10- 1 20 13 00 00 17 4E 9 9.6 9 02 53 87 00 11 27 -14 5 G 9 4 15 5.2 49. 0.0 0.0 0.0 49. 1.0 99. 56 1.0 10- 0 89 13 08 00 83 2E 9 6.3 8 02 85 04 24 23 11 -13 2 H 4 7 15 0.5 46. 0.0 0.0 0.0 44. 5.0 97. 51 4.5 10- 0 02 11 00 03 90 1E 6 7.6 2 03 72 27 00 79 55 -15 3 A 1 1 15 0.8 48. 0.0 0.0 -0. 48. 2.9 10 55 1.5 10- 0 27 12 00 00 48 9E 0.4 3.1 0 03 69 63 00 07 68 -14 6 B 2 1 4 15 1.2 49. 0.0 0.0 -0. 49. 4.6 10 55 2.3 10- 0 05 12 00 00 12 4E 0.2 9.4 7 03 06 63 00 02 64 -14 4 C 2 6 3 15 1.6 48. 0.0 0.4 0.0 48. 3.7 99. 55 1.8 10- 0 86 13 36 00 83 6E 9 6.5 2 03 39 11 36 27 19 -14 5 D 5 6 15 2.2 48. 0.0 0.1 0.0 48. 4.2 99. 55 1.4 10- 1 61 13 02 00 49 2E 8 3.2 5 03 47 46 06 44 63 -14 6 E 7 5 15 2.9 48. 0.0 0.0 -0. 48. 4.6 10 55 1.4 10- 0 66 12 00 00 68 4E 0.0 5.1 2 03 78 41 00 00 36 -14 0 F 2 5 0 15 3.7 48. 0.0 0.1 0.0 48. 5.7 99. 55 1.2 10- 1 63 13 04 00 54 6E 8 3.7 2 03 20 30 80 33 72 -14 6 G 5 8 15 5.1 48. 0.0 0.1 0.0 48. 3.7 99. 55 1.4 10- 9 66 13 62 00 60 8E 9 4.3 1 03 58 38 87 26 69 -14 4 H 9 7 HF bi- 15 0.3 15. 0.0 0.0 0.0 10. 8.9 70. 13 9.3 T3 otit 12- 0 07 13 00 15 59 7E 3 6.2 7 59 e 01 25 93 00 14 82 -16 2 A 6 9 15 0.6 51. 0.0 0.0 0.0 49. 2.7 95. 55 2.2 12- 0 66 16 55 08 17 6E 2 9.8 3 01 53 38 17 45 32 -14 9 B 7 8 15 0.9 51. 0.0 0.0 0.0 51. 8.8 99. 58 1.5 12- 0 95 15 00 00 82 5E 8 5.6 1 01 01 23 00 43 21 -14 4 C 9 5 15 1.2 53. 0.0 0.0 -0. 53. 1.0 10 60 1.2 12- 0 30 16 00 00 33 9E 0.1 0.2 4 01 51 44 00 01 91 -13 2 D 5 1 6 15 1.6 53. 0.0 0.0 0.0 53. 9.1 99. 60 1.1 12- 0 51 16 00 00 47 9E 9 1.5 8 01 90 06 00 14 64 -14 3 E 7 3 15 2.0 53. 0.0 0.0 -0. 53. 7.7 10 60 1.1 12- 1 51 15 00 00 52 8E 0.0 2.0 5 01 36 28 00 00 51 -14 0 F 3 4 8 15 2.6 53. 0.0 0.0 0.0 53. 9.2 99. 60 1.4 12- 0 64 15 00 00 59 3E 9 2.6 3 01 82 86 00 19 31 -14 5 G 1 1 15 3.8 53. 0.0 0.0 0.0 53. 1.3 10 59 0.9 12- 1 18 15 00 00 17 4E 0.0 8.6 9 01 65 85 00 04 57 -13 5 H 8 0 15 5.1 53. 0.0 0.0 0.0 53. 8.9 99. 59 1.7 12- 9 33 15 00 00 28 9E 9 9.7 9 01 73 78 00 16 98 -14 5 J 3 7 15 0.6 46. 0.0 0.0 0.0 44. 1.9 94. 51 3.6 12- 0 80 18 45 08 41 1E 9 2.7 6 02 20 27 37 09 63 -14 2 A 6 2 15 0.9 52. 0.0 0.0 0.0 52. 8.4 99. 58 1.4 12- 0 28 14 00 00 13 6E 7 8.6 0 02 70 38 00 51 56 -14 6 B 5 3 15 1.2 53. 0.0 0.0 0.0 53. 9.9 99. 59 2.5 12- 0 15 16 00 00 03 9E 8 7.3 2 02 88 19 00 42 48 -14 0 C 4 2 15 1.6 53. 0.0 0.0 0.0 53. 9.9 10 59 1.0 12- 0 03 16 73 00 03 1E 0.0 7.3 4 02 46 53 69 02 79 -14 3 D 7 8 15 2.2 53. 0.0 0.0 0.0 53. 1.1 10 59 1.0 12- 1 21 16 00 00 21 3E 0.0 8.9 3 02 00 52 00 00 04 -13 9 E 1 0 15 2.8 53. 0.0 0.0 0.0 52. 8.6 99. 59 1.0 12- 0 11 17 16 00 91 1E 6 6.1 3 02 87 80 24 71 14 -14 2 F 0 2 15 3.5 53. 0.0 0.0 0.0 53. 9.8 99. 60 5.3 12- 1 60 17 00 00 57 3E 9 2.5 6 02 60 51 00 10 71 -14 0 G 8 2 15 4.2 53. 0.0 0.0 -0. 53. 5.0 10 59 1.7 12- 1 09 13 00 00 25 8E 0.3 9.4 3 02 55 72 00 05 41 -14 1 H 9 4 3 15 5.2 52. 0.0 0.0 -0. 53. 8.1 10 59 1.3 12- 0 92 15 00 00 01 2E 0.2 7.1 6 02I 72 39 00 03 59 -14 2 9 0 3 15 0.6 48. 0.0 0.0 0.0 47. 3.4 96. 54 2.6 12- 0 91 14 00 05 29 1E 7 1.4 3 03 60 70 00 48 56 -14 2 A 0 7 15 0.9 52. 0.0 0.0 0.0 52. 9.4 10 59 1.4 12- 0 88 15 00 00 87 3E 0.0 5.7 9 03 94 35 00 05 52 -14 7 B 5 7 15 1.2 53. 0.0 0.0 0.0 53. 9.0 10 59 5.6 12- 0 11 14 00 00 10 1E 0.0 7.9 8 03 88 35 00 04 54 -14 8 C 9 5 15 1.6 53. 0.0 0.0 0.0 53. 7.4 99. 60 1.4 12- 0 38 14 00 00 31 8E 9 0.0 2 03 68 63 00 23 77 -14 1 D 1 6 15 2.2 53. 0.0 0.0 -0. 53. 9.1 10 59 1.3 12- 1 20 14 00 00 26 5E 0.1 9.5 8 03 77 13 00 01 48 -14 1 E 2 9 5 15 2.8 53. 0.0 0.0 0.0 53. 8.6 99. 59 1.9 12- 0 21 15 00 00 07 4E 7 7.6 6 03 02 33 00 47 10 -14 5 F 3 4 15 3.6 52. 0.0 0.0 -0. 52. 7.2 10 59 1.2 12- 0 81 14 00 00 90 9E 0.2 6.1 2 03 30 23 00 03 96 -14 0 G 0 3 7 15 5.1 53. 0.0 0.0 -0. 53. 6.2 10 59 2.0 12- 9 17 14 00 00 22 7E 0.1 9.1 8 03 21 54 00 01 24 -14 0 H 8 7 0 HF bi- 15 0.4 33. 0.0 1.6 0.0 30. 4.3 90. 36 4.0 T3 otit 13- 0 57 17 72 10 52 6E 8 7.4 2 61 e 01 07 87 80 86 82 -15 8 A 7 0 15 0.7 51. 0.0 0.0 0.0 51. 3.0 98. 58 1.4 13- 0 89 13 00 02 25 0E 8 0.1 4 01 37 88 00 15 70 -14 8 B 1 1 15 1.1 51. 0.0 0.2 0.0 51. 5.8 99. 58 1.1 13- 1 72 13 29 00 56 1E 7 3.1 8 01 37 81 65 62 53 -14 6 C 1 5 15 1.5 51. 0.0 0.0 -0. 52. 5.0 10 58 1.2 13- 0 99 12 00 00 03 0E 0.1 7.7 6 01 27 90 00 01 64 -14 1 D 9 5 7 15 2.0 52. 0.0 0.1 0.0 52. 4.7 99. 59 1.4 13- 1 41 12 60 00 36 7E 9 0.9 6 01 93 79 44 23 96 -14 2 E 1 8 15 2.6 51. 0.0 0.0 -0. 52. 4.7 10 58 1.3 13- 0 93 12 00 00 00 2E 0.1 7.3 8 01 84 21 00 02 41 -14 9 F 8 2 4 15 3.7 51. 0.0 0.1 0.0 51. 8.7 99. 58 1.4 13- 1 91 13 63 00 80 2E 8 5.4 1 01 48 40 72 44 38 -14 6 G 8 1 15 5.1 51. 0.0 0.2 -0. 51. 4.8 10 58 1.4 13- 9 91 12 39 00 94 4E 0.1 6.8 9 01 19 43 49 00 91 -14 6 H 8 4 2 15 0.6 50. 0.0 0.4 0.0 48. 1.8 96. 55 3.0 13- 0 61 16 16 06 69 9E 2 5.2 3 02 27 76 58 63 90 -14 5 A 4 6 15 0.9 51. 0.0 0.1 0.0 51. 4.0 99. 58 1.5 13- 0 91 14 50 01 63 2E 4 3.8 2 02 61 75 75 02 25 -14 1 B 1 7 15 1.2 51. 0.0 0.3 0.0 51. 3.9 99. 58 2.2 13- 0 60 14 20 00 41 9E 6 1.7 8 02 02 63 49 73 91 -14 5 C 5 6 15 1.6 51. 0.0 0.0 -0. 52. 3.9 10 58 1.5 13- 0 99 13 00 00 11 1E 0.2 8.4 0 02 94 61 00 03 29 -14 4 D 9 8 4 15 2.2 51. 0.0 0.0 -0. 51. 4.7 10 58 2.5 13- 1 93 13 00 00 99 7E 0.1 7.2 3 02 18 77 00 02 03 -14 6 E 7 0 9 15 2.9 51. 0.0 0.0 -0. 51. 6.1 10 58 1.1 13- 0 90 13 00 00 98 2E 0.1 7.1 0 02 50 92 00 02 07 -14 7 F 6 6 9 15 3.7 51. 0.0 0.0 -0. 51. 5.9 10 58 1.2 13- 1 69 13 00 00 78 9E 0.2 5.2 9 02 87 44 00 02 25 -14 6 G 9 8 6 15 5.1 51. 0.0 0.0 0.0 51. 2.4 99. 58 1.8 13- 9 93 13 57 00 76 1E 7 5.0 9 02 06 83 90 59 33 -14 7 H 8 7 15 0.6 39. 0.0 0.7 0.0 37. 1.0 94. 44 2.4 13- 0 77 16 10 07 49 7E 2 1.7 9 03 66 73 93 98 29 -14 8 A 2 9 15 0.9 52. 0.0 0.0 0.0 51. 4.2 99. 58 1.4 13- 0 00 13 00 00 86 6E 7 6.0 6 03 09 36 00 45 76 -14 8 B 2 7 15 1.2 52. 0.0 0.0 0.0 52. 5.2 10 59 1.2 13- 0 44 13 00 00 44 3E 0.0 1.6 9 03 43 37 00 01 07 -14 0 C 1 3 15 1.6 52. 0.0 0.2 0.0 52. 5.3 99. 58 1.4 13- 0 34 13 11 00 19 6E 7 9.1 4 03 14 73 95 59 02 -14 9 D 8 0 15 2.2 52. 0.0 0.2 0.0 52. 5.7 99. 59 1.4 13- 1 52 13 52 00 40 4E 8 1.3 0 03 46 98 42 49 92 -14 0 E 5 6 15 2.9 52. 0.0 0.1 0.0 52. 5.5 99. 59 1.1 13- 0 45 13 12 00 35 4E 8 0.7 4 03 82 61 53 40 31 -14 6 F 6 4 15 3.7 52. 0.0 0.0 -0. 52. 6.9 10 59 1.3 13- 1 38 13 06 00 40 6E 0.0 1.2 0 03 43 28 39 00 81 -14 9 G 8 8 3 15 5.1 52. 0.0 0.0 0.0 52. 1.0 99. 59 0.9 13- 9 53 14 21 00 50 5E 9 2.1 3 03 13 05 14 11 05 -13 7 H 0 9 HF bi- 15 0.4 47. 0.0 0.0 0.0 41. 7.8 86. 48 4.0 T3 otit 15- 0 60 18 00 21 27 4E 7 0.9 1 63 e 01 70 06 00 41 92 -15 2 B A 5 1 15 0.7 46. 0.0 0.0 0.0 46. 6.9 99. 53 1.2 15- 0 88 12 00 00 77 4E 8 6.2 3 01 26 42 00 36 54 -14 7 B 1 3 15 1.1 47. 0.0 0.0 0.0 46. 6.7 99. 53 1.2 15- 0 02 12 00 00 95 2E 9 8.0 9 01 59 71 00 24 56 -14 6 C 0 6 15 1.6 46. 0.0 0.0 -0. 46. 7.1 10 53 1.2 15- 0 85 11 00 00 95 2E 0.2 8.0 2 01 51 52 00 03 50 -14 5 D 3 4 3 15 2.1 47. 0.0 0.0 -0. 47. 4.6 10 54 1.3 15- 1 01 12 00 00 21 4E 0.4 0.6 3 01 74 12 00 06 39 -14 1 E 1 7 7 15 2.8 46. 0.0 0.0 -0. 47. 2.9 10 53 1.4 15- 0 84 11 00 00 05 1E 0.5 9.0 7 01 12 64 00 07 25 -14 2 F 5 2 8 15 3.7 46. 0.0 0.0 0.0 46. 1.7 99. 53 2.4 15- 1 93 13 00 00 65 5E 4 5.0 0 01 27 65 00 94 41 -14 7 G 6 8 15 5.1 46. 0.0 0.0 -0. 46. 2.3 10 53 1.8 15- 9 54 11 00 00 99 8E 1.0 8.4 2 01 28 19 00 15 39 -14 3 H 2 3 7 HF bi- 15 0.6 42. 0.0 0.6 0.0 40. 2.7 96. 47 1.4 T3 otit 15- 0 03 15 25 05 56 6E 4 3.5 7 63 e 02 94 34 79 22 23 -14 7 B A 4 3 15 0.8 46. 0.0 0.0 0.0 46. 6.0 99. 53 1.1 15- 0 98 13 00 00 83 8E 7 6.8 3 02 91 08 00 53 25 -14 3 B 4 2 15 1.1 46. 0.0 0.0 0.0 46. 6.9 99. 53 1.4 15- 0 93 12 00 00 87 4E 9 7.2 3 02 86 86 00 21 67 -14 7 C 8 8 15 1.6 46. 0.0 0.0 0.0 46. 6.8 99. 53 1.0 15- 0 85 12 05 00 76 5E 8 6.1 4 02 55 50 35 31 34 -14 5 D 3 4 15 2.1 46. 0.0 0.2 0.0 46. 8.4 99. 53 1.5 15- 1 87 12 23 00 80 7E 8 6.5 0 02 49 60 72 31 80 -14 9 E 2 4 15 3.2 46. 0.0 0.2 0.0 46. 5.3 99. 53 1.5 15- 0 83 12 77 00 78 4E 9 6.4 0 02 75 66 68 27 84 -14 0 F 9 0 15 5.1 46. 0.0 0.4 0.0 46. 6.1 99. 53 1.7 15- 9 81 12 27 00 76 4E 9 6.2 6 02 84 98 24 33 83 -14 0 G 4 8 15 0.6 39. 0.0 1.7 0.0 28. 1.2 72. 34 2.9 15- 0 04 22 16 36 30 0E 4 3.1 1 03 44 35 92 90 90 -14 5 A 7 8 15 0.8 45. 0.0 0.7 0.0 44. 3.1 98. 51 1.3 15- 0 42 14 02 02 76 3E 5 6.2 8 03 08 95 16 46 96 -14 7 B 5 2 15 1.1 46. 0.0 0.4 0.0 46. 5.1 99. 53 1.8 15- 0 64 12 42 00 62 6E 9 4.8 7 03 74 93 35 22 97 -14 2 C 8 4 15 1.6 47. 0.0 0.6 -0. 47. 3.6 10 53 2.0 15- 0 01 12 13 00 10 7E 0.1 9.5 6 03 98 31 77 00 60 -14 4 D 2 7 2 15 2.1 47. 0.0 0.2 -0. 47. 3.8 10 54 1.4 15- 1 21 12 68 00 34 1E 0.3 1.9 9 03 70 39 41 03 94 -14 5 E 3 5 1 15 3.2 47. 0.0 0.5 0.0 46. 4.6 99. 53 1.4 15- 0 04 12 68 00 97 0E 8 8.2 6 03 98 84 69 46 57 -14 5 F 2 0 15 5.1 46. 0.0 0.4 -0. 46. 5.1 10 53 1.2 15- 9 52 12 00 00 58 1E 0.1 4.3 3 03 02 06 55 00 49 -14 8 G 2 7 3 HF mu 15 0.5 60. -0. 0.0 0.0 54. 8.8 89. 61 23. T3 sco 16- 0 73 02 00 21 45 8E 7 0.8 79 63 vit 01 21 15 00 21 63 -16 8 B e A 2 8 6 15 0.9 50. 0.0 4.1 -0. 51. 2.7 10 57 8.3 16- 0 02 09 14 00 21 0E 2.1 9.7 5 01 76 10 60 24 70 -15 9 B 6 6 6 15 1.4 50. 0.0 0.3 0.0 49. 2.7 97. 56 2.9 16- 0 52 13 40 04 29 7E 5 1.1 6 01 58 48 05 29 67 -14 0 C 2 9 15 1.9 49. 0.0 0.0 0.0 49. 1.3 99. 56 1.1 16- 0 75 12 00 00 51 3E 5 3.1 1 01 71 07 00 83 05 -13 9 D 2 1 15 2.3 49. 0.0 0.0 0.0 49. 1.3 10 56 1.0 16- 1 21 11 00 00 20 2E 0.0 0.2 1 01 46 63 00 03 57 -13 1 E 5 0 15 2.8 49. 0.0 0.0 0.0 49. 3.0 99. 55 2.3 16- 0 14 11 00 00 03 4E 8 8.5 7 01 76 59 00 37 83 -14 7 F 1 9 15 3.7 49. 0.0 0.4 0.0 49. 2.6 99. 55 1.4 16- 1 43 12 80 01 13 7E 4 9.5 5 01 04 96 50 16 99 -14 7 G 8 2 15 5.1 49. 0.0 0.0 0.0 49. 1.4 10 56 1.0 16- 9 50 11 22 00 48 5E 0.0 2.9 4 01 81 94 30 08 71 -13 6 H 7 6 15 0.9 71. 0.0 0.0 0.0 49. 1.1 68. 56 24. 16- 0 84 45 00 75 39 8E 8 2.0 44 02 86 80 00 99 65 -15 8 A 6 8 15 1.4 49. 0.0 0.0 0.0 49. 3.6 98. 55 5.7 16- 0 63 11 00 01 06 6E 8 8.8 2 02 86 27 00 95 31 -15 2 B 5 7 15 1.7 49. 0.0 0.1 0.0 49. 4.2 99. 56 1.4 16- 0 65 11 35 00 38 0E 4 1.9 3 02 84 38 37 98 44 -14 6 C 2 8 15 2.0 49. 0.0 0.2 0.0 49. 3.8 99. 56 1.4 16- 1 75 12 34 01 39 9E 3 2.1 7 02 94 88 68 31 88 -14 0 D 5 5 15 2.4 49. 0.0 0.0 0.0 49. 1.2 99. 56 0.9 16- 0 28 11 00 00 25 1E 9 0.6 9 02 24 59 00 10 20 -13 7 E 7 3 15 3.7 49. 0.0 0.2 0.0 49. 2.4 10 56 1.6 16- 1 37 12 61 00 37 9E 0.0 1.9 4 02 74 17 65 09 90 -14 1 F 4 6 15 5.1 49. 0.0 0.0 0.0 49. 8.4 99. 56 1.5 16- 9 92 11 52 00 79 2E 7 6.0 2 02 58 80 21 44 98 -14 2 G 4 0 15 0.9 50. 0.0 1.0 0.0 45. 4.6 91. 52 5.5 16- 0 21 20 61 15 74 6E 0 5.9 3 03 01 51 09 52 09 -15 8 A 6 2 15 1.4 50. 0.0 0.3 0.0 48. 2.7 95. 55 2.0 16- 0 97 14 51 07 76 9E 6 5.9 8 03 86 20 40 62 62 -14 1 B 0 2 15 1.7 49. 0.0 0.0 0.0 49. 6.3 99. 55 1.5 16- 0 44 11 00 01 14 5E 4 9.6 0 03 41 82 00 01 61 -14 3 C 3 9 15 2.0 49. 0.0 0.0 0.0 49. 1.3 99. 56 1.0 16- 1 49 11 00 00 46 9E 9 2.7 3 03 75 80 00 10 62 -13 6 D 1 2 15 2.4 49. 0.0 0.0 0.0 49. 8.8 99. 56 1.0 16- 0 57 11 00 00 51 0E 9 3.2 8 03 44 64 00 19 89 -14 8 E 7 9 15 3.7 49. 0.0 0.0 0.0 49. 9.5 10 56 1.3 16- 1 46 11 13 00 44 5E 0.0 2.5 6 03 85 63 78 07 75 -14 8 F 2 8 15 5.2 49. 0.0 0.0 0.0 49. 2.1 99. 56 1.7 16- 0 44 11 13 00 40 8E 9 2.1 7 03 10 68 47 12 52 -13 6 G 2 9 Note

Data from the southern Brasília belt. See text for details of sample location and description. Journal of the Virtual Explorer, 2004 Volume 17 Paper 2 http://virtualexplorer.com.au/

Final stages of the Brasiliano Orogenesis in SE Brazil: U-Pb and 40Ar/39Ar evidence for overprinting of the Brasília Belt by the Ribeira Page 20 Belt Tectonics