Structure of the Southern Cordillera Oriental (Argentinean Andes)
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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. -
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. -
Mesozoic to Tertiary Evolution of the Southwestern Proto-Pacific Gondwana Margin
University of Sydney, PhD Thesis, Kayla T. Maloney, 2012. The University of Sydney School of Geosciences Mesozoic to Tertiary evolution of the southwestern proto-Pacific Gondwana margin Kayla T. Maloney 2012 Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy The University of Sydney School of Geosciences Division of Geology and Geophysics Madsen Building (F09) Sydney, NSW, 2006 Australia University of Sydney, PhD Thesis, Kayla T. Maloney, 2012. i DECLARATION I declare that this thesis is less than 100,000 words in length, and that the work contained in this thesis has not been submitted for a higher degree at any other university or institution. Kayla T. Maloney August, 2012 PREFACE This PhD thesis consists of a collection of papers that are published or prepared for submission with international peer-reviewed journals appropriate to the discipline of geology. The publications form part of an integrated project and are presented in an order that represents the related elements of a connected thesis. The thesis contains an introductory section that provides an outline of the thesis, a summary of the contribution of the work to the field of geology, and a critical evaluation of the role of the thesis in informing further research in the field. Common themes in the papers are tied together and a discussion and conclusion of the whole thesis is presented at the end. No animal or ethical approvals were needed during the completion of this study. Data and interpretations in the thesis are the work of the author except where stated in the text. -
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. -
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. -
Provenance Study on Neoproterozoic Rocks of Nw Argentina: Puncoviscana Formation – First Results
U N I V E R S I D A D D E C O N C E P C I Ó N DEPARTAMENTO DE CIENCIAS DE LA TIERRA 10° CONGRESO GEOLÓGICO CHILENO 2003 PROVENANCE STUDY ON NEOPROTEROZOIC ROCKS OF NW ARGENTINA: PUNCOVISCANA FORMATION – FIRST RESULTS ZIMMERMANN, U.1 1Dep.of Geol., RAU University, Auckland Park 2092, South Africa [email protected] INTRODUCTION Since more than 20 years the western border of Gondwana is object of controversies related to the basic question if crustal growth is related to terrane accretion or to “recycling” of the same crustal rocks during the Vendian and Lower Paleozoic. Different hypotheses were developed regarding the evolution of that margin. One of the key element to understand the crustal evolution, is the Vendian to Lower Cambrian so-called PVF. Turner (1960) described rock successions in northwestern Argentina (Fig. 1) of Pre-Ordovician age comprising greywackes and sand- and siltstones, but dominated by pelites as the PVF. Afterwards, it was established that mostly all Vendian to Lower Cambrian very-low to low grade metasedimentary rocks in the region are classified, such as Suncho, Negro Peinado or La Cébila Formation (e.g. comp. in Aceñolaza et al., 1988), are equivalents of the PVF. Widely distributed medium- to high-grade metasedimentary rocks (Fig. 1), those rocks were interpreted as exhumed deeper crustal levels of the PVF (Willner, 1990). Other authors deny this opinion and interpret the different metamorphic rocks related to different events, consequently of different ages (Mon and Hongn, 1990). Based on only punctual petrographic work, the depositional area was defined as a passive margin based on petrography and mainly major element geochemistry (Jezek, 1990, Willner et al., 1985, Rossi Toselli et al., 1997), or on preliminary trace element data (Do Campo and Ribeiro Guevara, 2002). -
Along-Strike Variation in Structural Styles and Hydrocarbon Occurrences, Subandean Fold-And-Thrust Belt and Inner Foreland, Colombia to Argentina
The Geological Society of America Memoir 212 2015 Along-strike variation in structural styles and hydrocarbon occurrences, Subandean fold-and-thrust belt and inner foreland, Colombia to Argentina Michael F. McGroder Richard O. Lease* David M. Pearson† ExxonMobil Upstream Research Company, Houston, Texas 77252, USA ABSTRACT The approximately N-S–trending Andean retroarc fold-and-thrust belt is the locus of up to 300 km of Cenozoic shortening at the convergent plate boundary where the Nazca plate subducts beneath South America. Inherited pre-Cenozoic differences in the overriding plate are largely responsible for the highly segmented distribution of hydrocarbon resources in the fold-and-thrust belt. We use an ~7500-km-long, orogen- parallel (“strike”) structural cross section drawn near the eastern terminus of the fold belt between the Colombia-Venezuela border and the south end of the Neuquén Basin, Argentina, to illustrate the control these inherited crustal elements have on structural styles and the distribution of petroleum resources. Three pre-Andean tectonic events are chiefl y responsible for segmentation of sub- basins along the trend. First, the Late Ordovician “Ocloyic” tectonic event, recording terrane accretion from the southwest onto the margin of South America (present-day northern Argentina and Chile), resulted in the formation of a NNW-trending crustal welt oriented obliquely to the modern-day Andes. This paleohigh infl uenced the dis- tribution of multiple petroleum system elements in post-Ordovician time. Second, the mid-Carboniferous “Chañic” event was a less profound event that created mod- est structural relief. Basin segmentation and localized structural collapse during this period set the stage for deposition of important Carboniferous and Permian source rocks in the Madre de Dios and Ucayali Basins in Peru. -
From Rodinia to Gondwana
GEOSCIENCE FRONTIERS 3(2) (2012) 137e145 available at www.sciencedirect.com China University of Geosciences (Beijing) GEOSCIENCE FRONTIERS journal homepage: www.elsevier.com/locate/gsf 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 Available online 3 December 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. -
Maquetación 1
1º Reunión Virtual de Comunicaciones de la Asociación Paleontológica Argentina 25–26 de noviembre de 2020 Libro de Resúmenes ASOCIACIÓN PALEONTOLÓGICA ARGENTINA COMISIÓN DIRECTIVA Presidenta Juliana Sterli Vicepresidenta Julia Desojo Secretario Javier Echevarría Prosecretaria Lucía Balarino Tesorero Pablo Gallina Protesorero Diego Balseiro Vocales Mónica Buono Jose Carballido Federico J. Degrange Paula Muzzopappa Damián Pérez Verónica Vennari doi: 10.5710/PEAPA.28.04.2021.392 R1 PE-APA 21 (1R) – Libro de Resúmenes La Asociación Paleontológica Argentina se enorgullece en presentar la 1º Reunión Virtual de Comunicaciones de la APA, 1º RVCAPA, en un año donde, por razones de público conocimiento, no se han podido concretar de forma presencial las reuniones y congresos organizados por nuestra comunidad. La misma se llevó adelante del 25 al 26 de noviembre de 2020, en el marco de los festejos por el Día del/a Paleontólogo/a. El objetivo principal fue mantener el contacto y la comunicación entre los miembros de la comunidad paleontológica y en especial motivar a estudiantes de grado, posgrado y posdoctorado a presentar y discutir los resultados de sus investigaciones en esta reunión. También participaron investigadores/as, técnicos/as y paleoartistas en todas las instancias de sus carreras. Esta reunión contó con conferencias de especialistas nacionales e internacionales y con comunicaciones libres en formato de pósteres virtuales. El acceso a la reunión, en su totalidad, fue a través de enlaces de la plataforma Google Meet, en videoconferencias a distancia . R2 PE-APA 21 (1R) – Libro de Resúmenes CONFERENCIAS R3 PE-APA 21 (1R) – Libro de Resúmenes R4 PE-APA 21 (1R) – Libro de Resúmenes RESÚMENES LOS TYPOTHERIA (NOTOUNGULATA, MAMMALIA) DE LA LOCALIDAD CRUCES INFINITOS DEL MIOCENO MEDIO DEL CHUBUT (PATAGONIA ARGENTINA) BREnDA M. -
Chapter 5 the Pre-Andean Phases of Construction of the Southern Andes Basement in Neoproterozoic-Paleozoic Times
133 Chapter 5 The Pre-Andean phases of construction of the Southern Andes basement in Neoproterozoic-Paleozoic times Nemesio Heredia; Joaquín García-Sansegundo; Gloria Gallastegui; Pedro Farias; Raúl E. Giacosa; Fernando D. Hongn; José María Tubía; Juan Luis Alonso; Pere Busquets; Reynaldo Charrier; Pilar Clariana; Ferrán Colombo; Andrés Cuesta; Jorge Gallastegui; Laura B. Giambiagi; Luis González-Menéndez; Carlos O. Limarino; Fidel Martín-González; David Pedreira; Luis Quintana; Luis Roberto Rodríguez- Fernández; Álvaro Rubio-Ordóñez; Raúl E. Seggiaro; Samanta Serra-Varela; Luis A. Spalletti; Raúl Cardó; Victor A. Ramos Abstract During the late Neoproterozoic and Paleozoic times, the Southern Andes of Argentina and Chile (21º-55º S) formed part of the southwestern margin of Gondwana. During this period of time, a set of continental fragments of variable extent and allochtony was successively accreted to that margin, resulting in six Paleozoic orogenies of different temporal and spatial extension: Pampean (Ediacaran-early Cambrian), Famatinian (Middle Ordovician-Silurian), Ocloyic (Middle Ordovician-Devonian), Chanic (Middle Devonian-early Carboniferous), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies culminate with collisional events, with the exception of the Tabarin and a part of the Gondwanan orogenies that are subduction-related. Keywords Paleozoic, Southern Andes, Pampean orogen, Ocloyic orogen, Famatinian orogen, Chanic orogen, Gondwanan orogen, Tabarin orogen. 133 134 1 Introduction In the southern part of the Andean Cordillera (21º-55º S, Fig. 1A) and nearby areas, there are Neoproterozoic (Ediacaran)-Paleozoic basement relicts of variable extension. This basement has been involved in orogenic events prior to the Andean orogeny, which is related to the current configuration of the Andean chain (active since the Cretaceous). -
Uncorrected Proofs
N. Jb. Geol. Paläont. Abh. Article Stuttgart, July 2012 Basin evolution of the margin of Gondwana at the Neoproterozoic/ Cambrian transition: the Puncoviscana Formation of Northwest Argentina Alejandro J. Toselli, Guillermo F. Aceñolaza, Hubert Miller, Christopher Adams, Florencio G. Aceñolaza, and Juana N. Rossi With 4 figures Toselli, A.J., AceñolAzA, G.F., Miller, H., Adams, c., AceñolAzA, F.G. & rossi, J.N. (2012): Basin evolution of the margin of Gondwana at the Neoproterozoic/Cambrian transition: the Puncoviscana Formation of Northwest Argentina. – N. Jb. Geol. Paläont. Abh., 265: 000-000; Stuttgart. Abstract: The Puncoviscana Formation is an important stratigraphic sequence of sandstones and shales, with intercalated conglomerates, limestones and volcanic rocks. It was deposited at the Neo- proterozoic-Cambrian boundary in a shallow basin on the western margin of Gondwana. Trace fos- sils of the Puncoviscana Formation s.l. are represented by the Oldhamia and Nereites ichnoassocia- tions and the geographical distribution of assemblages are alignedproofs as parallel belts, with a shallower eastern Nereites association and a deeper western Oldhamia association. They represent different temporal levels on the evolution of the basin. Detrital zircon spectra display a wide range of ages, which indicate their provenance from Neoproterozoic to Cambrian source areas as well as Meso- to Paleoproterozoic basement units, exhibiting typical Gondwanan ages. Thick limestone banks are interbedded in the Puncoviscana Formation s.l. that included the siliciclastic sequences, with very low- to medium-metamorphic grade. δ13C values for the limestones vary from -1.57 to +3.40/00 VPDB, while in the Sierras Pampeanas, δ13C values vary from +2.6 to +80/00 VPDB. -
Review of the Cambrian Pampean Orogeny of Argentina; a 2 Displaced Orogen Formerly Attached to the Saldania Belt of 3 South Africa? 4 5 César Casqueta*, Juán A
1 Review of the Cambrian Pampean orogeny of Argentina; a 2 displaced orogen formerly attached to the Saldania Belt of 3 South Africa? 4 5 César Casqueta*, Juán A. Dahlquistb, Sebastián O. Verdecchiab, Edgardo G. 6 Baldob, Carmen Galindoa, Carlos W. Rapelac, Robert, J. Pankhurstd, Matias 7 M. Moralesb, Juán A. Murrab, C. Mark Fanninge 8 9 a Departamento de Petrología y Geoquímica, Facultad de Ciencias Geológicas, Instituto de 10 Geología Económica (CSIC), Universidad Complutense, 28040 Madrid, Spain1 11 b Centro de Investigaciones en Ciencias de la Tierra (CICTERRA), CONICET, Universidad 12 Nacional de Córdoba, Av. Vélez Sarsfield 1611, Pab. Geol., X5016CGA Córdoba, Argentina 13 c Centro de Investigaciones Geológicas, CONICET, Universidad Nacional de la Plata, 1900 La 14 Plata, Argentina 15 d Visiting Research Associate, British Geological Survey, Keyworth, Nottingham NG12 5GG, 16 UK 17 e Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, 18 Australia 19 20 21 Keywords: Pampean orogeny; Saldanian orogeny; Sierras Pampeanas; Gondwana; Mara 22 terrane; collisional orogeny 23 24 25 Abstract 26 27 The Pampean orogeny of northern Argentina resulted from Early Cambrian oblique 28 collision of the Paleoproterozoic MARA block, formerly attached to Laurentia, with the 29 Gondwanan Kalahari and Rio de la Plata cratons. The orogen is partially preserved 30 because it is bounded by the younger Córdoba Fault on the east and by the Los Túneles 31 Ordovician shear zone on the west. In this review we correlate the Pampean Belt with 32 the Saldania orogenic belt of South Africa and argue that both formed at an active 33 continental margin fed with sediments coming mainly from the erosion of the 34 Brasiliano–Pan-African and East African–Antarctica orogens between ca.