38. Structural and Stratigraphic Evolution of the Sumisu Rift, Izu-Bonin Arc1
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Styles and Scales of Structural Inheritance Throughout Continental Rifting
Styles and Scales of Structural Inheritance throughout Continental Rifting Examples from the Great South Basin, New Zealand Thomas B. Phillips* & Ken J. McCaffrey Durham University *[email protected] Rationale Continental crust comprises distinct crustal units and intruded magmatic material brought together throughout multiple tectonic events Samsu al., (2018) et Beniest et al., (2018) • Crustal/lithospheric strength may • Strain may initially localise in weaker influence the rift structural style and areas of lithosphere, rather than at the physiography boundaries between different domains How do lateral crustal strength contrasts, along with prominent crustal boundaries, influence rift structural style and physiography? • The Great South Basin, New Zealand forms atop basement comprising multiple distinct terranes and magmatic intrusions. • The extension direction during rifting is parallel to the terrane boundaries, such that all terranes experience extensional strain Geological evolution of Zealandia A C Area of focus - 1. Cambrian- Cret. subduction along Great South Basin S. margin of Gondwana 3. Gondwana breakup Aus-NZ and NZ-West Antarctica. Formation of rift basins on cont. shelf B D 2. Ribbon-like accretion of distinct island-arc- related terranes 4. Formation of oppositely dipping subduction zones and offsetting of Uruski. (2010) basement terranes Courtesy of IODP Basement beneath the Great South Basin Work in progress/Preliminary • Distinct basement terranes of varying strength related to Island Arc system accreted -
A New Look at Maverick Basin Basement Tectonics Michael Alexander, Integrated Geophysics Corporation
Bulletin of the South Texas Geological Society A New Look at Maverick Basin Basement Tectonics Michael Alexander, Integrated Geophysics Corporation 50 Briar Hollow Lane, Suite 400W Houston, Texas 77027 Technical Article Technical ABSTRACT concepts regarding the evolution and relationships of the various sub-basins and regional faulting. The current Eagle Ford play in South Texas has More importantly, it could stimulate new ideas regenerated exploration interest in the Maverick about exploring for several potential new and Basin area. The greater Maverick Basin is shown deeper plays in the Jurassic and pre-Jurassic to consist of several sub-basins, each having a section. unique tectonic character. Three broad Cretaceous basins overlie narrow Jurassic basins that are considered to be part of a left-stepping rift system INTRODUCTION associated with a regional southeast-northwest shear zone. Much of the current literature considers the greater Maverick Basin to be a classic Jurassic rift valley. The northern Maverick area contains two deep and Some papers describe the northern sub-basin as a narrow Jurassic sub-basins, the Moody and the deep Jurassic rift bounded to the southwest by Paloma, both of which trend southeast-northwest. northeast-directed folds or anticlines produced by This northern area is separated from the central Laramide compression from Mexico. Other Maverick area by a southwesterly trend of papers describe the central sub-basin as a interpreted basement highs associated with the Cretaceous-Jurassic half-graben with the Chittim Edwards Arch. A Jurassic rift basin, the Chittim Anticline located over its steep northeast flank. Basin, is located in the central Maverick area. -
Philippine Sea Plate Inception, Evolution, and Consumption with Special Emphasis on the Early Stages of Izu-Bonin-Mariana Subduction Lallemand
Progress in Earth and Planetary Science Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Lallemand Lallemand Progress in Earth and Planetary Science (2016) 3:15 DOI 10.1186/s40645-016-0085-6 Lallemand Progress in Earth and Planetary Science (2016) 3:15 Progress in Earth and DOI 10.1186/s40645-016-0085-6 Planetary Science REVIEW Open Access Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Serge Lallemand1,2 Abstract We compiled the most relevant data acquired throughout the Philippine Sea Plate (PSP) from the early expeditions to the most recent. We also analyzed the various explanatory models in light of this updated dataset. The following main conclusions are discussed in this study. (1) The Izanagi slab detachment beneath the East Asia margin around 60–55 Ma likely triggered the Oki-Daito plume occurrence, Mesozoic proto-PSP splitting, shortening and then failure across the paleo-transform boundary between the proto-PSP and the Pacific Plate, Izu-Bonin-Mariana subduction initiation and ultimately PSP inception. (2) The initial splitting phase of the composite proto-PSP under the plume influence at ∼54–48 Ma led to the formation of the long-lived West Philippine Basin and short-lived oceanic basins, part of whose crust has been ambiguously called “fore-arc basalts” (FABs). (3) Shortening across the paleo-transform boundary evolved into thrusting within the Pacific Plate at ∼52–50 Ma, allowing it to subduct beneath the newly formed PSP, which was composed of an alternance of thick Mesozoic terranes and thin oceanic lithosphere. -
Ishikukaepsl10.Pdf
Earth and Planetary Science Letters 294 (2010) 111–122 Contents lists available at ScienceDirect Earth and Planetary Science Letters journal homepage: www.elsevier.com/locate/epsl Migrating shoshonitic magmatism tracks Izu–Bonin–Mariana intra-oceanic arc rift propagation O. Ishizuka a,b,⁎, M. Yuasa a, Y. Tamura b, H. Shukuno b, R.J. Stern c, J. Naka b, M. Joshima a, R.N. Taylor d a Institute of Geology and Geoinformation, Geological Survey of Japan/AIST, Central 7, 1-1-1, Higashi, Tsukuba, Ibaraki, 305-8567, Japan b IFREE, JAMSTEC, 2-15 Natsushima, Yokosuka, Kanagawa, 237-0061, Japan c Dept. of Geosciences, University of Texas at Dallas, Richardson TX 75083-0688, USA d National Oceanography Centre, Southampton, European Way, Southampton, SO14 3ZH, UK article info abstract Article history: The southernmost Izu–Bonin arc and northernmost Mariana arc are characterized by K-rich and shoshonitic Received 22 November 2009 lavas, referred to as the alkalic volcano province (AVP). These compositions are unusual for intra-oceanic arcs Received in revised form 6 March 2010 and the interpretation of the AVP is controversial. Rifting to form the Mariana Trough back-arc basin occurs Accepted 12 March 2010 just south of the AVP although back-arc seafloor spreading has not begun. Here we report the results of Available online 9 April 2010 dredge sampling of the West Mariana Ridge (WMR) in the region of rift propagation; this recovered Editor: R.W. Carlson exclusively medium K to shoshonitic basalts that show clear arc-like geochemical signatures. Ar–Ar ages of WMR shoshonitics systematically young northward. -
53. Petrologic Evolution of the Mariana Arc and Back-Arc Basin System— a Synthesis of Drilling Results in the South Philippine Sea1
53. PETROLOGIC EVOLUTION OF THE MARIANA ARC AND BACK-ARC BASIN SYSTEM— A SYNTHESIS OF DRILLING RESULTS IN THE SOUTH PHILIPPINE SEA1 James H. Natland, Deep Sea Drilling Project, Scripps Institution of Oceanography, La Jolla, California and John Tarney, Department of Geology, University of Leicester, LEI 7RH, United Kingdom ABSTRACT The results of Deep Sea Drilling Project Leg 60 pertaining to the petrologic evolution of the Mariana Trough and Mariana arc are summarized in Part I. The rocks recovered at five principal sites are exceptionally diverse, including gabbros and calc-alkalic andesites derived from the West Mariana Ridge; fresh and hydrothermally altered basalts in the Mariana Trough; and interbedded boninites and arc tholeiites in the forearc region between the modern arc and the trench. Part I outlines the stratigraphy, alteration, and petrology of these rock suites and summarizes hypotheses on their origin. Part II integrates these results with those of previous DSDP legs in the region, and with island sampling, to present a composite 40-m.y. history of the Mariana arc system. Arc volcanism began in the Eocene, probably as a result of a change to the west in the motion of the Pacific plate. A north-south-trending fracture zone was transformed into a trench-subduction complex, trapping a portion of the Pacific plate in the Philippine Sea. The crust of this basin, drilled in Hole 447 (Leg 59), has the composition of typical ocean floor basalt. The earliest Eocene arc was built up dominantly of arc tholeiite and boninitic lavas, with lesser calc-alkalic lavas, based on the results of Leg 60 drilling at Sites 458 and 459 in the forearc region; Leg 59, Site 448, on the Palau-Kyushu Ridge; and exposures on the islands of Palau, Guam, and Saipan. -
Pamphlet to Accompany
Geologic and Geophysical Maps of the Eastern Three- Fourths of the Cambria 30´ x 60´ Quadrangle, Central California Coast Ranges Pamphlet to accompany Scientific Investigations Map 3287 2014 U.S. Department of the Interior U.S. Geological Survey This page is intentionally left blank Contents Contents ........................................................................................................................................................................... ii Introduction ..................................................................................................................................................................... 1 Interactive PDF ............................................................................................................................................................ 2 Stratigraphy ..................................................................................................................................................................... 5 Basement Complexes ................................................................................................................................................. 5 Salinian Complex ..................................................................................................................................................... 5 Great Valley Complex ............................................................................................................................................ 10 Franciscan Complex ............................................................................................................................................. -
Mariana Magmatic Arc Hiyoshi Volcanic Complex and Iwo Jima
Mariana Magmatic Arc Hiyoshi Volcanic Complex and Iwo Jima: Bloomer, S. H., Stern, R. J., Fisk, E., and Geschwind, C. H. "Shoshonitic volcanism in the northern Mariana Arc: 1. Petrographic and major and trace element characteristics." J. Geophys. Res., 94, 4469-4496, 1989. Ishizuka, O., Yuasa, M., Tamura, Y., Shukuno, H., Stern, R.J., Naka, J, Joshima, M., and Taylor, R.N., 2010. Migrating shoshonitic magmatism tracks Izu-Bonin- Mariana intra-oceanic arc rift propagation. Earth Planet. Sci. Lett. 294, 111-122 Lin, P.-N., Stern, R. J., and Bloomer, S. H. "Shoshonitic Volcanism in the Northern Mariana Arc: 2. Large-Ion Lithophile and Rare Earth Element Abundances - Evidence for the Source of Incompatible Element Enrichments in Intra-Oceanic Arcs." J. Geophys. Res., 94, 4497-4514, 1989. Meen, J.K., Stern, R.J., and Bloomer, S.H.,1998. Evidence for magma mixing in the Mariana arc system The Island Arc 7, 443-459. Stern, R. J., Bloomer, S. H., Lin, P.-N., Ito, E., and Morris, J. 1988. Shoshonitic magmas in nascent arcs: New evidence from submarine volcanoes in the northern Marianas. Geology, 16, p. 426-430. Stern, R. J., Smoot, N. C., and Rubin, M., 1984. Unzipping of the Volcano Arc, Japan." Tectonophysics, 102, p. 153-174. Sun, C.-H., Stern, R.J., Yoshida, T., and Kimura, J.-I., 1998. Fukutoku-oka-no-ba Volcano: A new perspective on the Alkalic Volcano Province in the Izu-Bonin- Mariana arc The Island Arc 7, 432-442. Kasuga cross-chain (KXN): Stern, R. J., Jackson, M. C., Fryer, P., and Ito, E. -
Deep Sea Drilling Project Initial Reports Volume 59
38. EVOLUTION OF THE SOUTH PHILIPPINE SEA: DEEP SEA DRILLING PROJECT LEG 59 RESULTS Robert B. Scott, Department of Geology, Texas A&M University, College Station, Texas Loren Kroenke, Hawaii Institute of Geophysics, University of Hawaii, Honolulu, Hawaii Guram Zakariadze,1 Institute of Geology, Georgian Academy of Sciences, Tbilisi, U.S.S.R. and Anatoli Sharaskin, Vernadsky Institute of Geochemistry, U.S.S.R. Academy of Sciences, 117334, Moscow, U.S.S.R. INTRODUCTION (Hussong, Uyeda et al., 1978). Only through an integra- tion of all these investigations can a coherent evolution Several prominent inactive and active arcs and of the inactive arcs and marginal basins of the South marginal basins lie within the confines of the South Philippine Sea be constructed. Philippine Sea (Fig. 1). These are, from west to east, the Because timing of events in the arcs and basins is fun- inactive West Philippine Basin, Palau-Kyushu Ridge, damental to any evolutionary scheme, modern plank- Parece Vela Basin, and West Mariana Ridge and the ac- tonic biozonation is used. The zonations used by Ingle tive Mariana Trough and Mariana Ridge. The two most (1975) on Leg 31, by Martini (this volume) on Leg 59, acceptable hypotheses suggested for the origin of these and by Hussong, Uyeda et al. (in press) on Leg 60, how- marginal basins are (1) the entrapment of preexisting ever, all differ somewhat. For a discussion of these dif- oceanic crust and (2) the formation of new oceanic crust ferences see the biostratigraphic synthesis by Martini et by back-arc sea-floor spreading. al. -
Steeply Dipping Basement Faults and Associated Structures of the Santander Massif, Eastern Cordillera, Colombian Andes
Geologia Colombian a No. 18, 1993 Steeply Dipping Basement Faults and Associated Structures of the Santander Massif, Eastern Cordillera, Colombian Andes ANDREAS KAMMER Departamento de Geocienciss, Universidad Nacional de Colombia, Apartado 14490, Bogota, Colombia KAMMER, A. (1993): Steeply Dipping Basement Faults and Associated Structures of the Santander Massif, Eastern Cordillera, Colombian Andes.- Geologia Colombiana, 18, pp. 47 - 64,12 figs, 2 Tablas, Bogota. RESUMEN vollzogen, an denen Relikte des Sedimentmantels eingekeilt wurden und sich Halbqraben bildeten. Das EI Macizo de Santander expone ampliamente el Bruchmuster wurde weitgehend von einer jurassischen basamento andino "viejo" y estil Iimitado hacia sus Dehnungstektonik ererbt. Die Neogenen cuencas de "antepais" par fallas inversas mayores. Abschiebungen kormen einer vertikalen Fallas mas Internas, aunque con buzamientos fuertes, Hebungstektonik zugeordnet werden, bei der, bedingt pueden clasificarsecomo faUasnormales que hundieron durch die facherartige Anordnung der BrOche, zentrale la cobertera sedimentaria a 10largo de semi - grabenes. Teile der Aufwolbung des Massivs absinken mussten. EI patron de estas fallas estil heredado en gran medida Ein leicht abgeandertes Modell wird an einem schmalen, a partir de una tectcnlca [uraeica de extension. La kompressiven Grundgebirgshorst erprobt, WO, wahrend tectonlca extensiva Ne6gena puede integrarse a un der Hebung Randbereiche direkt Ober den inversen modelo de levantamiento vertical, que par el arreglo en BrOchen einbrachen und sich charakteristische abanico de sus fallas indujo un componente de Synklinalen bildeten. dilatacion lateral. Este modelo estil modificado para un estrecho antiforme fallado, el alto de Malaga, en donde 1. INTRODUCTION el espacio Iimitado no permitio el hundimiento de su parte central, pero en dondeel ajuste del bloque colgante Section modelling of the Eastern Cordillera has become a las fallas inversas divergentes se hizo por el colapso increasingly popular in the past years and different attempts de sinclinales marginales. -
Crustal Structure of the Southwestern Colombian Caribbean Margin
CRUSTAL STRUCTURE OF THE SOUTHWESTERN COLOMBIAN CARIBBEAN MARGIN Geological interpretation of geophysical data Dissertation zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) Vorgelegt dem Rat der Chemisch-Geowissenschaftlichen Fakultät der Friedrich-Schiller-Universität Jena von Diplom-Geologin Adriana Maria Mantilla Pimiento geboren am 7. Februar 1971 in Bucaramanga, Kolumbien Gutachter Prof. Dr. Gerhard Jentzsch Prof. Dr. Jonas Kley Friedrich-Schiller-Universität Jena, Insitut für Geowissenschaften Tag der öffentlichen Verteidigung: 28. November 2007 To Carlos Arturo, Richard, Myriam, José Manuel and Monica with love and gratitude. Contents CONTENTS Abstract vii Zusammenfassung ix Resumen xi 1 INTRODUCTION AND OUTLINE 1 1.1 Aims and methods 1 1.2 Previous works 1 1.3 Thesis outline 4 2 REGIONAL SETTING OF NW COLOMBIA 7 2.1 Caribbean tectonic overview 7 2.2 Tectonic framework of northern Colombia 10 2.3 Geology of study area 15 2.3.1 Sinú Fold Belt 15 2.3.2 San Jacinto Fold Belt 15 2.3.3 Lower Magdalena Valley Basin 17 2.3.4 Romeral Fault System 17 2.4 Stratigraphic framework 18 3 2D STRUCTURAL CONFIGURATION 23 3.1 Colombian Caribbean Basin (trench domain) 23 3.2 The active accretionary domain 24 3.3 Outer high (older accretionary domain) 25 3.4 Forearc domain 28 4 GRAVITY AND MAGNETIC ANOMALIES 33 4.1 Bouguer anomaly map 33 i Contents 4.2 Regional isostatic map 35 4.3 Qualitative interpretation of magnetic anomalies 37 4.3.1 Magnetic total-field intensity map 37 4.3.2 Reduce-to-Pole map 39 5 3D FORWARD GRAVITY -
Mechanics of Thick-Skinned Variscan
+ Models CRAS2A 2812 1–13 1 C. R. Geoscience xxx (2009) xxx–xxx http://france.elsevier.com/direct/CRAS2A/ 2 Tectonics 43 Mechanics of thick-skinned Variscan overprinting of 5 Cadomian basement (Iberian Variscides) 6 a a, a a 7 António Ribeiro , José Munhá *, António Mateus , Paulo Fonseca , b c d b 8 Eurico Pereira , Fernando Noronha , José Romão , José Rodrigues , Paulo Castro b, Carlos Meireles b, Narciso Ferreira b 9 10 a Department Geologia and CEGUL, Faculdade de Ciências, Universidade de Lisboa, Ed. C6, Piso 3, Campo Grande, 11 1749-016 Lisboa, Portugal 12 b Department de Geologia, Laboratório Nacional de Energia e Geologia, 4466-956 S. Mamede Infesta, Portugal 13 c Department Geologia and CEGUP, Faculdade de Ciências, Universidade do Porto, Rua do Campo Alegre 687, 14 4169-007 Porto, Portugal 15 d Department Geologia, Laboratório Nacional de Energia e Geologia, Apartado 7586, 16 2721-866 Alfragide, Portugal 17 Received 19 February 2008; accepted after revision 25 November 2008 18 211920 Written on invitation of the Editorial Board 22 Abstract 23 24 Remnants of the Cadomian basement can be found in the Iberian Variscides (IBVA) in several key sectors of its autochthonous 25 units (composed of Neoproterozoic to Lower Palaeozoic metasedimentary sequences) and within the Continental Allochthonous 26 Terrane (CAT). Comprehensive characterization of these critical exposures shows that the prevailing features are related to major 27 geological events dated within the age range of 620–540 Ma. Indeed, near the Cambrian–Ordovician boundary, the IBVA Internal 28 Zones experienced pervasive basement thinning and cover thickening, reflecting diffusive displacement of intracratonic rifting that 29 continued until Lower Devonian times. -
33. Geochemistry of Igneous Rocks Recovered from a Transect Across the Mariana Trough, Arc, Fore-Arc
33. GEOCHEMISTRY OF IGNEOUS ROCKS RECOVERED FROM A TRANSECT ACROSS THE MARIANA TROUGH, ARC, FORE-ARC, AND TRENCH, SITES 453 THROUGH 461, DEEP SEA DRILLING PROJECT LEG 601 D. A. Wood,2 N. G. Marsh,2 J. Tarney,2 J.-L. Joron,3 P. Fryer,4 and M. Treuil3 ABSTRACT Major and trace element analyses are presented for 110 samples from the DSDP Leg 60 basement cores drilled along a transect across the Mariana Trough, arc, fore-arc, and Trench at about 18°N. The igneous rocks forming breccias at Site 453 in the west Mariana Trough include plutonic cumulates and basalts with calc-alkaline affinities. Basalts recovered from Sites 454 and 456 in the Mariana Trough include types with compositions similar to normal MORB and types with calc-alkaline affinities within a single hole. At Site 454 the basalts show a complete compositional transition between normal MORB and calc-alkaline basalts. These basalts may be the result of mixing of the two magma types in small sub-crustal magma reservoirs or assimilation of calc-alkaline, arc-derived vitric tuffs by normal MORB magmas during eruption or intrusion. A basaltic andesite clast in the breccia recovered from Site 457 on the active Mariana arc and samples dredged from a seamount in the Mariana arc are calc-alkaline and similar in composition to the basalts recovered from the Mariana Trough and West Mariana Ridge. Primitive island arc tholeiites were recovered from all four sites (Sites 458-461) drilled on the fore-arc and arc-side wall of the trench. These basalts form a coherent compositional group distinct from the Mariana arc, West Mariana arc, and Mariana Trough calc-alkaline lavas, indicating temporal (and perhaps spatial?) chemical variations in the arc magmas erupted along the transect.