Uncorrected Proofs
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Redalyc.Sr, C and O Isotope Composition of Marbles from The
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España Murra, J.A.; Baldo, E.G.; Galindo, C.; Casquet, C.; Pankhurst, R.J.; Rapela, C.W.; Dahlquist, J. Sr, C and O isotope composition of marbles from the Sierra de Ancasti, Eastern Sierras Pampeanas, Argentina: age and constraints for the Neoproterozoic-Lower Paleozoic evolution of the proto- Gondwana margin Geologica Acta: an international earth science journal, vol. 9, núm. 1, marzo, 2011, pp. 79-92 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50522124008 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.9, Nº 1, March 2011, 79-92 DOI: 10.1344/105.000001645 Available online at www.geologica-acta.com Sr, C and O isotope composition of marbles from the Sierra de Ancasti, Eastern Sierras Pampeanas, Argentina: age and constraints for the Neoproterozoic–Lower Paleozoic evolution of the proto-Gondwana margin 1 1 2 2 3 4 1 J.A. MURRA E.G. BALDO C. GALINDO C. CASQUET R.J. PANKHURST C.W. RAPELA J. DAHLQUIST 1 CICTERRA (Universidad Nacional de Córdoba - Conicet) Av. Vélez Sarsfield 1611, 5016 Córdoba, Argentina. Murra E-mail: [email protected] Baldo E-mail: [email protected] Dahlquist E-mail: [email protected] 2 Departamento. Petrología y Geoquímica Facultad de Ciencias Geológicas, Inst. -
Early Evolution of the Proto-Andean Margin of South America
Early evolution of the Proto-Andean margin of South America C. W. Rapela Centro de Investigaciones Geológicas, Universidad Nacional de La Plata, Calle 1 No. 644, 1900 La Plata, Argentina R. J. Pankhurst British Antarctic Survey, Cambridge CB30ET, United Kingdom C. Casquet Departamento de Petrología y Geoquímica, Universidad Complutense, 28040 Madrid, Spain E. Baldo J. Saavedra CSIC, Instituto de Agrobiología y Recursos Naturales, 37071 Salamanca, Spain C. Galindo Departamento de Petrología y Geoquímica, Universidad Complutense, 28040 Madrid, Spain ABSTRACT INTRODUCTION From a detailed study of a 500 km transect in the Sierras Pampeanas, central-west Argen- The evolution of the Gondwana margin pro- tina, two pre-Silurian tectono-magmatic episodes are recognized and defined, each culminating posed here is based on new geochemical, isotopic, in micro-continental collisions against the proto-Andean margin of Gondwana. The Pampean petrological, and sedimentological data from a orogeny started in Early Cambrian time with short-lived subduction, indicated by ca. 535 Ma 500 km traverse across the Eastern Sierras Pam- calc-alkaline granitoids. Following Pampean terrane collision, burial to granulite facies condi- peanas and Precordillera (Fig. 1). Pre-Silurian tions (ca. 9 kbar) generated widespread migmatites and ca. 520 Ma highly peraluminous gran- metamorphic and magmatic history is inferred ites in the Eastern Sierras Pampeanas. After brief quiescence, a second major episode, the from (1) dating by conventional U-Pb on abraded Famatinian orogeny, started with subduction ca. 490 Ma, forming a wide continental arc and zircons, U-Pb SHRIMP analyses, and whole-rock ensialic backarc basin. This heralded the approach of Laurentia to Gondwana, during which Rb-Sr and K-Ar, (2) thermo-barometry based on the Precordillera terrane separated from the southern Appalachian region, finally colliding with microprobe mineral analyses, and (3) Nd and Sr Gondwana in Silurian–Devonian time. -
The Cambrian System in Northwestern Argentina: Stratigraphical and Palaeontological Framework Discussion Geologica Acta: an International Earth Science Journal, Vol
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España Buatois, L.A.; Mángano, M.G. Discussion and reply: The Cambrian System in Northwestern Argentina: stratigraphical and palaeontological framework Discussion Geologica Acta: an international earth science journal, vol. 3, núm. 1, 2005, pp. 65-72 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50530107 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.3, Nº1, 2005, 65-72 Available online at www.geologica-acta.com Discussion and reply: The Cambrian System in Northwestern Argentina: stratigraphical and palaeontological framework Discussion L.A. BUATOIS and M.G. MÁNGANO CONICET- INSUGEO Casilla de correo 1 (correo central), 4000 San Miguel de Tucumán, Argentina. Present address: Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada. Buatois E-mail: [email protected] INTRODUCTION this rift corresponds to the early above-mentioned Punco- viscana basin”. This gives the wrong impression that there As part of the Special Issue on “Advances in the is some sort of consensus on this topic, which is incorrect. knowledge of the Cambrian System” edited by himself, Interestingly enough, this southern rift branch is perpendi- Aceñolaza (2003) attempted to summarize present know- cular to the Gondwana Pacific trench (see his figure 3), an ledge on the Cambrian of northwest Argentina. -
GSA TODAY • Radon in Water, P
Vol. 8, No. 11 November 1998 INSIDE • Field Guide Editor, p. 5 GSA TODAY • Radon in Water, p. 10 • Women Geoscientists, p. 12 A Publication of the Geological Society of America • 1999 Annual Meeting, p. 31 Gas Hydrates: Greenhouse Nightmare? Energy Panacea or Pipe Dream? Bilal U. Haq, National Science Foundation, Division of Ocean Science, Arlington, VA 22230 ABSTRACT Recent interest in methane hydrates has resulted from the recognition that they may play important roles in the global carbon cycle and rapid climate change through emissions of methane from marine sediments and permafrost into the atmosphere, and in causing mass failure of sediments and structural changes on the continental slope. Their presumed large volumes are also consid- ered to be a potential source for future exploitation of methane as a resource. Natural gas hydrates occur widely on continental slope and rise, stabilized in place by high hydrostatic pressure and frigid bottom-temperature condi- tions. Change in these conditions, Figure 1. This seismic profile, over the landward side of Blake Ridge, crosses a salt diapir; the profile has either through lowering of sea level or been processed to show reflection strength. The prominent bottom simulating reflector (BSR) swings increase in bottom-water temperature, upward over the diapir because of the higher conductivity of the salt. Note the very strong reflections of may trigger the following sequence of gas accumulations below the gas-hydrate stability zone and the “blanking” of energy above it. Bright events: dissociation of the hydrate at its Spots along near-vertical faults above the diapir represent conduits for gas venting. -
A History of Proterozoic Terranes in Southern South America: from Rodinia to Gondwana
+ MODEL GEOSCIENCE FRONTIERS -(-) (2011) 1e9 available at www.sciencedirect.com China University of Geosciences (Beijing) GEOSCIENCE FRONTIERS journal homepage: www.elsevier.com/locate/gsf REVIEW A history of Proterozoic terranes in southern South America: From Rodinia to Gondwana C. Casquet a,*, C.W. Rapela b, R.J. Pankhurst c, E.G. Baldo d, C. Galindo a, C.M. Fanning e, J.A. Dahlquist d, J. Saavedra f a Departamento de Petrologıa y Geoquımica, IGEO (Universidad Complutense, CSIC), 28040 Madrid, Spain b Centro de Investigaciones Geologicas (CONICET-UNLP), 1900 La Plata, Argentina c Visiting Research Associate, British Geological Survey, Keyworth, Nottingham NG12 5GG, United Kingdom d CICTERRA (CONICET-UNC), 5000 Cordoba, Argentina e Research School of Earth Sciences, The Australian National University, Canberra, Australia f Instituto de Agrobiologıa y Recursos Naturales CSIC, 37071 Salamanca, Spain Received 3 August 2011; accepted 8 November 2011 KEYWORDS Abstract The role played by Paleoproterozoic cratons in southern South America from the Mesopro- Paleoproterozoic; terozoic to the Early Cambrian is reconsidered here. This period involved protracted continental amal- Cratons; gamation that led to formation of the supercontinent Rodinia, followed by Neoproterozoic continental Grenvillian; break-up, with the consequent opening of Clymene and Iapetus oceans, and finally continental Neoproterozoic rifting; re-assembly as Gondwana through complex oblique collisions in the Late Neoproterozoic to Early SW Gondwana assembly Cambrian. The evidence for this is based mainly on a combination of precise U-Pb SHRMP dating and radiogenic isotope data for igneous and metamorphic rocks from a large area extending from the Rio de la Plata craton in the east to the Argentine Precordillera in the west and as far north as Arequipa in Peru. -
Cactus Explorer the first Free On-Line Journal for Cactus and Succulent Enthusiasts
TheCactus Explorer The first free on-line Journal for Cactus and Succulent Enthusiasts 1 Schlumbergera opuntioides 2 Parodia mammulosa Number 13 3 Explorers Weekend 2014 ISSN 2048-0482 4 Crassulaceae at Lyon B.G. December 2014 5 Schlumbergera truncata The Cactus Explorer ISSN 2048-0482 Number 13 December 2014 THE POSITION OF PARODIA TURECEKIANA IN THE PARODIA MAMMULOSA COMPLEX In this article, Giovanna Anceschi & Alberto Magli discuss Parodia turecekiana R. Kiesling, part of the Parodia mammulosa (Lemaire) Taylor complex. Photographs by the authors Fig.1 Parodia mammulosa (turecekiana populations). Uruguay, Rio Negro, Nuevo Berlin. 27 Jan 2014, A&M 966 During the seven months of our 2013/2014 Parodia turecekiana R. Kiesling was one of journey, out of the 70 new taxa we investigated our “black sheep”. In fact, before this year’s in habitat for a forthcoming classification in the happy discovery, we failed to find the above Cactusinhabitat system, 11 belong to the genus mentioned taxon of the Pampa Biome on three Parodia Spegazzini (precisely, 10 are Andean occasions. The first time was in November taxa and one from the Pampa Biome). Parodia 2008, in Uruguay, Dpt. Río Negro, on Ruta 25, being one of our genera of preference, during between Bellaco and Young, following the our next journey we hope to find or deepen the reference R. Kiesling 8368 (Kiesling 1995, 67: knowledge of the last four taxa that will allow 18). The second time, again in November 2008, us to have a complete overview of Parodia s.l., in Uruguay, Dpt. Río Negro, Young, northwest based on study experience in the habitats of all of Young, locality Paso Uleste, in the its components. -
Provenance and Tectonic Implications of Orán Group Foreland Basin
Basin Research (2015) 1–17, doi: 10.1111/bre.12139 Provenance and tectonic implications of Oran Group foreland basin sediments,RıoIruyacanyon,NW Argentina (23° S) William H. Amidon,* Lisa V. Luna,* George B. Fisher,† Douglas W. Burbank,† Andrew R. C. Kylander-Clark† and Ricardo Alonso‡ *Middlebury College Geology Department, Middlebury, VT, USA †Earth Research Institute, University of California, Santa Barbara, CA, USA ‡Departamento de Geologıa, Universidad Nacional de Salta, Salta, Argentina ABSTRACT Foreland basins are important recorders of tectonic and climatic processes in evolving mountain ranges. The Rıo Iruya canyon of NW Argentina (23° S) exposes ca. 7500 m of Oran Group foreland basin sediments, spanning over 8 Myr of near continuous deposition in the Central Andes. This study presents a record of sedimentary provenance for the Iruya Section in the context of a revised stratigraphic chronology. We use U-Pb zircon ages from six interbedded ash layers and new magnet- ostratigraphy to constrain depositional ages in the section between 1.94 and 6.49 Ma, giving an aver- 1 age sedimentation rate of 0.93 0.02 (2r) km MyrÀ . We then pair U-Pb detrital zircon dating Æ with quartz trace-element analysis to track changes in sedimentary provenance from ca. 7.6 to 1.8 Ma. Results suggest that from ca. 7.6 to ca. 6.3 Ma, the Iruya watershed did not tap the Salta Group or Neogene volcanics that are currently exposed in the eastern Cordillera and Puna margin. One explanation is that a long-lived topographic barrier separated the eastern Puna from the foreland for much of the mid-late Miocene, and that the arrival of Jurassic-Neogene zircons records regional tectonic reactivation at ca. -
Volume 8, Issue 2, 2017 ISSN 2191-3099 This Document Was Published in Pdf Format: August 19Th 2017
Schütziana The Gymnocalycium Online Journal Volume 8, Issue 2, 2017 ISSN 2191-3099 This document was published in pdf format: August 19th 2017 Content Papsch, Wolfgang Editorial p. 2 Marx, Ulf p. 3-10 Franz Strigl – 80 years and still young at heart Kulhánek, Tomáš Papsch, Wolfgang On the Distribution of Gymnocalycium platense p. 11-23 (Spegazzini) Britton & Rose (Cactaceae) Kulhánek, Tomáš Gymnocalycium alenae Kulhánek, a new species p. 24-38 from the northern part of province Córdoba Published: August 19th 2017 Legal notice Publisher: WORKING GROUP SCHÜTZIANA, Fichtenweg 43, 14547 Fichtenwalde, Germany Editorial team and responsible for the content: www.schuetziana.org/contact.php Mario Wick, 14547 Fichtenwalde, Fichtenweg 43, Germany, [email protected] Massimo Meregalli, 10123 Torino, V. Accademia Albertina, 17, Italia, [email protected] Wolfgang Papsch, 8401 Kalsdorf, Ziehrenweg 6, Austria, [email protected] Tomáš Kulhánek, 67201 Moravský Krumlov, Tylova 673, Czech Republic, [email protected]. SCHÜTZIANA is the journal of the WORKING GROUP SCHÜTZIANA. Source of supply: SCHÜTZIANA is available only as a pdf-file via World Wide Web and can be downloaded from: www.schuetziana.org/download.php. The content of the respective article expresses the opinion of the author and need not being in agreement with the opinion of the WORKING GROUP SCHÜTZIANA. The issues of SCHÜTZIANA are free of charge and may be distributed freely. The content and the pictures of the articles of SCHÜTZIANA are property of the author and may not be used for other purposes than reading, printing and storing without permission. © 2017 WORKING GROUP SCHÜTZIANA. -
Andean Flat-Slab Subduction Through Time
Andean flat-slab subduction through time VICTOR A. RAMOS & ANDRE´ S FOLGUERA* Laboratorio de Tecto´nica Andina, Universidad de Buenos Aires – CONICET *Corresponding author (e-mail: [email protected]) Abstract: The analysis of magmatic distribution, basin formation, tectonic evolution and structural styles of different segments of the Andes shows that most of the Andes have experienced a stage of flat subduction. Evidence is presented here for a wide range of regions throughout the Andes, including the three present flat-slab segments (Pampean, Peruvian, Bucaramanga), three incipient flat-slab segments (‘Carnegie’, Guan˜acos, ‘Tehuantepec’), three older and no longer active Cenozoic flat-slab segments (Altiplano, Puna, Payenia), and an inferred Palaeozoic flat- slab segment (Early Permian ‘San Rafael’). Based on the present characteristics of the Pampean flat slab, combined with the Peruvian and Bucaramanga segments, a pattern of geological processes can be attributed to slab shallowing and steepening. This pattern permits recognition of other older Cenozoic subhorizontal subduction zones throughout the Andes. Based on crustal thickness, two different settings of slab steepening are proposed. Slab steepening under thick crust leads to dela- mination, basaltic underplating, lower crustal melting, extension and widespread rhyolitic volcan- ism, as seen in the caldera formation and huge ignimbritic fields of the Altiplano and Puna segments. On the other hand, when steepening affects thin crust, extension and extensive within-plate basaltic flows reach the surface, forming large volcanic provinces, such as Payenia in the southern Andes. This last case has very limited crustal melt along the axial part of the Andean roots, which shows incipient delamination. -
Variabilidad Morfológica Y Modelos Arqueológicos
1 El presente trabajo se orientó al estudio de la variación craneofacial de los grupos humanos que habitaron el sector austral de las Sierras Pampeanas y llanuras circundantes en tiempos prehispánicos desde una perspectiva que combina análisis morfológicos cuali-cuantitativos y análisis basados en la morfometría geométrica. Como objetivos específicos se planteó: a) caracterizar morfológicamente colecciones arqueológicas inéditas de restos óseos, b) estudiar la variación craneofacial de las mencionadas colecciones a partir de análisis de morfometría geométrica, c) establecer relaciones genéticas entre las poblaciones de la región central del país y demás regiones geográfico-ecológicas de Argentina y Sudamérica (Andes, Amazonia, Gran Chaco, Patagonia-Tierra del Fuego), d) poner a prueba diferentes modelos sobre las posibles vías de poblamiento del centro del país. Los resultados sugieren importantes similitudes a nivel de morfología craneal y variación epigenética entre muestras principalmente del lado oriental de las sierras –actual territorio de la provincia de Córdoba- y poblaciones del centro y Noreste de Patagonia, y región pampeana. Teniendo en cuenta los resultados generales, consideramos que el poblamiento de la región austral de las Sierras Pampeanas se relaciona con aquel ocurrido desde el Noreste del país, siguiendo un derrotero general Norte-Sur a través del Litoral Atlántico. Mariana Fabra Doctora en Historia (Facultad de Filosofía y Humanidades, Universidad Nacional de Córdoba, Argentina) y Magister en Antropología (FFyH, UNC), se desempeña actualmente como Investigadora Adjunta del Consejo Nacional de Investigaciones Científicas y Técnicas. Es Profesora Asistente la licenciatura en Antropología (Departamento de Antropología, Área Antropología Biológica, FFyH, UNC). Ha dirigido diversos proyectos de investigación (PIP CONICET, PID MiNCyT Córdoba), sobre temáticas vinculadas al poblamiento de la región central de Argentina y el estilo de vida de las poblaciones originarias del centro del país desde una perspectiva bioarqueológica. -
From Rodinia to Gondwana
A history of Proterozoic terranes in southern South America: From Rodinia to Gondwana C. Casquet a,*, c.w. Rapela b, R.J. Pankhurst c, E.G. Baldo d, C. Galindo a, C.M. Fanning e, J.A. Dahlquist d, J. Saavedra f a Departamento de Petrologia y Geoquimica, ICEO (Universidad Complutense, CSIC), 28040 Madrid, Spain b Centra de Investigaciones Geologicas (CONICET-UNLP), 1900 La Plata, Argentina C 'Visiting Research Associate, British Geological SUlVey, Keyworth, Nottingham NG12 SCC, United Kingdom d CICTERRA (CONICET-UNC), 5000 Cordoba, Argentina e Research School of Earth Sciences, The Australian National University, Canberra, Australia f Instituto de Agrobiologia y Recursos Naturales CSIC, 37071 Salamanca, Spain KEYWORDS Abstract The role played by Paleoproterozoic cratons in southern South America from the Mesopro Paleoproterozoic; terozoic to the Early Cambrian is reconsidered here. This period involved protracted continental amal Cratons; gamation that led to formation of the supercontinent Rodinia, followed by N eoproterozoic continental Grenvillian; break-up, with the consequent opening of Clymene and Iapetus oceans, and finally continental Neoproterozoic rifting; re-assembly as Gondwana through complex oblique collisions in the Late Neoproterozoic to Early SW Gondwana assembly Cambrian. The evidence for this is based mainly on a combination of precise U-Pb SHRMP dating and radiogenic isotope data for igneous and metamorphic rocks from a large area extending from the Rio de la Plata craton in the east to the Argentine Precordillera in the west and as far north as Arequipa in Peru. Our interpretation of the paleogeograpbical and geodynamic evolution invokes a hypothetical Paleoproterozoic block (MARA) embracing basement ultimately older than 1.7 Ga in the Western Sierras 1. -
The Proto-Andean Margin of Gondwana: an Introduction
Downloaded from http://sp.lyellcollection.org/ by guest on September 29, 2021 The proto-Andean margin of Gondwana: an introduction R. J. PANKHURST 1 & C. W. RAPELA 2 1 British Antarctic Survey, c/o NERC Isotope Geosciences Laboratory, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG, UK 2 Centro de Investigaciones Geol6gicas, Universidad Naeional de la Plata, 644 Calle No. 1, 1900 La Plata, Argentina Abstract: A basic background is presented for the discussion of the Early Palaeozoic geology of western Argentina covered by this book. This includes the definition and terminology of orogenic cycles on this part of the Gondwana margin, represented by the Eastern Sierras Pampeanas. The Pampean orogeny (Early Cambrian) relates to an intense but short-lived period of terrane collision predating the rifting of the Precordillera terrane from Laurentia. The Famatinian cycle is predominantly represented by intense subduction- related magmatism of Early-Middle Ordovician age, developed on the continental margin of Gondwana during the rifting and drifting of the Precordillera terrane. The Grenvillian basement of the latter is further exemplified by a new Rb-Sr whole-rock isochron age of 1021 + 12Ma for orthogneisses from the Western Sierras Pampeanas. A mid-Ordovician granite in this area (dated at 481 4-6 Ma by U-Pb ion microprobe data) may be related to rifting while the Precordillera terrane was still attached to Laurentia. A divergence of opinion is pointed out between some authors in this book who favour mid-Ordovician collision of the Precordillera with Gondwana, and others who place it much latter, in Silurian or Devonian times.