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A Revised Lithostratigraphy of the Sierra Baguales, Magallanes Basin
A revised lithostratigraphy of the Sierra Baguales, Magallanes Basin Enrique Bostelmann 1, Jacobus P. Le Roux 2, Ana Vasquez 2, Nestor Gutiérrez 2, José Luis Oyarzún 3, Catalina Carreño 2, Teresa Torres 4, Rodrigo Otero 5, Andrea Llanos 4, C. Mark Fanning 6, Sven N. Nielsen 7, Francisco Hervé 2,8 1Museo Nacional de Historia Natural, CC. 399, 11.000. Montevideo, Uruguay 2Departamento de Geología, Universidad de Chile / Centro de Excelencia en Geotermia de los Andes, Casilla 13518, Santiago, Chile 3Parque Geológico y Paleontológico, La Cumbre-Baguales 4Departamento de Producción Agrícola, Facultad de Ciencias Agronómicas, Universidad de Chile, Correo 1004, Santiago, Chile 5Área Paleontología, Museo Nacional de Historia Natural. Casilla 787, Santiago, Chile 6Research School of Earth Sciences, The Australian National University, Mills Road, Canberra, ACT 0200, Australia 7Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Str. 10, 24118 Kiel, Germany 8Departamento de Geología, Universidad Andrés Bello, Santiago, Chile Abstract We present a new lithostratigraphic scheme zircons in the Loreto Formation have been dated at for the Sierra Baguales north of Torres del Paine based 36.48±0.47–36.73±0.5 Ma (Otero et al., 2012), on recent field work, which shows that the stratigraphy whereas zircons in the Río Baguales Formation have of the Lake Argentino region of Argentina is duplicated yielded an age of 40.48±0.37 Ma (Le Roux, 2012). here. The former Río Baguales Formation probably The Loreto Formation was named as early as 1931 by correlates with the Man Aike Formation of Argentina and also in part with the Loreto Formation of the Keidel and Hemmer, whereas its stratigraphic Brunswick Peninsula, so that the name Loreto is equivalents were named much later: the Río Baguales retained for this unit. -
Chronology and Geology of an Early Miocene
Andean Geology 41 (3): 507-528. September, 2014 Andean Geology doi: 10.5027/andgeoV41n3-a02 formerly Revista Geológica de Chile www.andeangeology.cl Chronology and geology of an Early Miocene mammalian assemblage in North of South America, from Cerro La Cruz (Castillo Formation), Lara state, Venezuela: implications in the ‘changing course of Orinoco River’ hypothesis *Ascanio D. Rincón1, Andrés Solórzano1, Mouloud Benammi2, Patrick Vignaud2, H. Gregory McDonald3 1 Laboratorio de Paleontología, Centro de Ecología, Instituto Venezolano de Investigaciones Científicas (IVIC), Caracas, Venezuela. [email protected]; [email protected] 2 Institut de Paléoprimatologie, Paléontologie Humaine, Evolution et Paleonviroments, UMR CNRS 7262-INEE, Université de Poitiers, France. [email protected]; [email protected] 3 Museum Management Program, National Park Service, 1201 Oakridge Drive, Fort Collins, Colorado 80525, U.S.A. [email protected] * Corresponding author: [email protected] ABSTRACT. In general the geology of paleontological sites in Venezuela is poorly known. With the purpose of im- proving this knowledge we describe the geology of the Castillo Formation (Late Oligocene to Early Miocene) at Cerro La Cruz locality, in Lara state, Venezuela, that contains several records of vertebrate and invertebrate fauna. Litholog- ically, the Cerro La Cruz sequence is composed by alternating packages of siliciclastic and carbonate sediments, with a predominance of mudstone. The paleoenvironment is inferred as a mainly near-shore marine complex that could be associated with regressive and transgressive phases. Nevertheless, into the middle part of the Cerro La Cruz outcrops two levels containing at least six mammalian remains were found, confirming the early continental mammal assemblage in Venezuela. -
The Venezuelan Hydrocarbon Habitat, Part 1: Tectonics, Structure, Palaeogeography and Source Rocks
Journal of Petroleum Geology, vo1.23(1), January 2000, pp 5-53. 5 THE VENEZUELAN HYDROCARBON HABITAT, PART 1: TECTONICS, STRUCTURE, PALAEOGEOGRAPHY AND SOURCE ROCKS K. H. James* Venezuela forms part of an important hydrocarbon province, defined by the presence of prolific Cretaceous source rocks, which extends across northern South America. By early 1997, the country had produced 53 billion barrels of oil. Reserves are estimated to total 73 billion barrels of oil and 146 TCF of gas with 250 billion barrels recoverable in the Heavy Oil Belt. Most reserves are located within the intermontane Maracaibo and foreland Barinas-Apure and Eastern Venezuela BasinxThey correspond to more than 1.5 trillion BOE originally in place. The province S hydrocarbon history began with a broad passive margin over which the sea transgressed throughout much ofthe Cretaceous. Limestones and shales followed basal sands and included rich source rocks. Convergence between the distal part of the area and the Caribbean Plate created an active margin that migrated southwards, so that flysch and wildflysch followed the transgressive facies. The process culminated in Lute Cretaceous to Middle Eocene orogeny with the emplacement of southward-vergent nappes and the development of northward-deepeningforedeeps. Flysch and wildflysch formed in the north while important deltaic - paralic reservoir sands accumulated in the south. Major phases of hydrocarbon generationfrom Jurassic-Cretaceoussource rocks occurred across the entire margin of northern South America during the orogeny. They are recorded by Jurassic - Middle Cretaceous graphitic marbles, schists and quartzites (metamorphosed, organic limestones and shales and oil-bearing sandstones) in the Coastal and Northern Ranges of Venezuela and Trinidad. -
(Early Miocene) in Lago Posadas, Southwestern Patagonia, Argentina
Andean Geology 46 (2): 383-420. May, 2019 Andean Geology doi: 10.5027/andgeoV46n2-3128 www.andeangeology.cl Sedimentology and fossil vertebrates of the Santa Cruz Formation (early Miocene) in Lago Posadas, southwestern Patagonia, Argentina *José I. Cuitiño1, Sergio F. Vizcaíno2, 3, M. Susana Bargo2, 4, Inés Aramendía5 1 Instituto Patagónico de Geología y Paleontología (IPGP, CCT CONICET-CENPAT). Boulevard Brown 2915, Puerto Madryn (9120), Chubut, Argentina. [email protected] 2 División Paleontología de Vertebrados, Museo de La Plata, Unidades de Investigación Anexo Museo, 60 y 122, La Plata (1900), Argentina. [email protected]; [email protected] 3 Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) Argentina. 4 Comisión de Investigaciones Científicas (CIC), calle 526 entre 10 y 11, 1900 La Plata-Buenos Aires, Argentina. 5 Instituto Patagónico para el Estudio de Ecosistemas Continentales (IPEEC, CCT CONICET-CENPAT). Boulevard Brown 2915, Puerto Madryn (9120), Chubut, Argentina. [email protected] * Corresponding author: [email protected] ABSTRACT. Lago Posadas is located at the foot of the Southern Patagonian Andes, in southwestern Argentina, where the early Miocene Santa Cruz Formation (SCF) shows thick and laterally continuous exposures. This region has been scarcely explored for fossil vertebrates since the first efforts by J.B. Hatcher in 1898-99. In this contribution, we performed sedimentologic and paleontological studies in order to reconstruct depositional -
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Crust-mantle interactions and generation of silicic melts: insights from the Sarmiento Complex, southern Patagonian Andes Mauricio Calderón Departamento de Geología, Universidad de Chile, Francisco Hervé Casilla 13518, Correo 21,Santiago, Chile [email protected] [email protected] Umberto Cordani Centro de Pesquisas Geocronológicas, Universidade de São Paulo, Rua do Lago 562, Cidade Universitaria, São Paulo, CEP 05508-900, Brazil [email protected] Hans-Joachim Massonne Institut für Mineralogie und Kristallchemie, Universität Stuttgart, Azenbergstrasse 18, D-70174, Stuttgart, Germany [email protected] ABSTRACT A Late Jurassic seafloor remnant of the Rocas Verdes basin in southern Chile, the Sarmiento Complex (ca. 52°S), bears lithological layers with bimodal meta-igneous rocks appropriate for a comprehensive investigation of magma genesis in part of a lateral lithological transition from continental rifting to initial seafloor spreading. Metamorphosed mafic ε rocks collected from different layers in the ophiolite pseudostratigraphy and a plagiogranite have positive Nd150 values ε (+ 1 and +2). Granophyres, which are crosscut by ophiolitic mafic dikes, have negative Nd150 values (-5). Dacitic dikes ε within thick successions of pillow basalt have the least negative Nd150 values (-3 and -4). Although mafic and felsic igneous rocks show contrasting isotopic signatures, thermochemical modeling (EC-AFC) suggests they can share a common origin. Models consider an arbitrary composition of the crustal assimilant (mostly metapelite with an average ε Nd150 value of -7) and evaluate the feasibility for generation of silicic melts through the interaction of mafic magmas and metasedimentary rocks. A quantitative evaluation of basaltic magma contaminated by crustal wall rocks requires a Ma*/ Mc (mass of anatectic melt/ mass of cumulates) ratio of 0.04. -
Sedimentary Record of Andean Mountain Building
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/321814349 Sedimentary record of Andean mountain building Article in Earth-Science Reviews · March 2018 DOI: 10.1016/j.earscirev.2017.11.025 CITATIONS READS 12 2,367 1 author: Brian K. Horton University of Texas at Austin 188 PUBLICATIONS 5,174 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Petroleum Tectonic of Fold and Thrust Belts View project Collisional tectonics View project All content following this page was uploaded by Brian K. Horton on 15 December 2018. The user has requested enhancement of the downloaded file. Earth-Science Reviews 178 (2018) 279–309 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Invited review Sedimentary record of Andean mountain building T Brian K. Horton Department of Geological Sciences and Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78712, United States ARTICLE INFO ABSTRACT Keywords: Integration of regional stratigraphic relationships with data on sediment accumulation, provenance, Andes paleodrainage, and deformation timing enables a reconstruction of Mesozoic-Cenozoic subduction-related Fold-thrust belts mountain building along the western margin of South America. Sedimentary basins evolved in a wide range of Foreland basins structural settings on both flanks of the Andean magmatic arc, with strong signatures of retroarc crustal Orogeny shortening, flexure, and rapid accumulation in long-lived foreland and hinterland basins. Extensional basins also Sediment provenance formed during pre-Andean backarc extension and locally in selected forearc, arc, and retroarc zones during Late Stratigraphy Subduction Cretaceous-Cenozoic Andean orogenesis. -
Burdigalian Deposits of the Santa Cruz Formation in the Sierra Baguales, Austral (Magallanes) Basin: Age, Depositional Environment and Vertebrate Fossils
Andean Geology 40 (3): 458-489, September, 2013 Andean Geology doi: 10.5027/andgeoV40n3-a0410.5027/andgeoV40n3-a?? formerly Revista Geológica de Chile www.andeangeology.cl Burdigalian deposits of the Santa Cruz Formation in the Sierra Baguales, Austral (Magallanes) Basin: Age, depositional environment and vertebrate fossils J. Enrique Bostelmann1, 2, Jacobus P. Le Roux3, Ana Vásquez3, Néstor M. Gutiérrez3, José Luis Oyarzún4, Catalina Carreño3, Teresa Torres5, Rodrigo Otero2, Andrea Llanos5, C. Mark Fanning6, Francisco Hervé3, 7 1 Museo Nacional de Historia Natural, 25 de Mayo 582, Montevideo, Uruguay. [email protected] 2 Red Paleontológica U-Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Avda. Las Palmeras 3425, Ñuñoa, Santiago,Chile. [email protected] 3 Departamento de Geología, Universidad de Chile, Centro de Excelencia en Geotermia de los Andes, Plaza Ercilla 803, Santiago, Chile. [email protected]; [email protected]; [email protected]; [email protected]; [email protected] 4 Callejón Pedro Méndez, Huerto N° 112, Puerto Natales, Chile. [email protected] 5 Departamento de Producción Agrícola, Facultad de Ciencias Agronómicas, Universidad de Chile, Avda. Santa Rosa N° 11315, La Pintana, Santiago, Chile. [email protected]; [email protected] 6 Research School of Earth Sciences, The Australian National University, Building 142 Mills Road, ACT 0200, Canberra, Australia. [email protected] 7 Escuela de Ciencias de la Tierra, Universidad Andrés Bello, Salvador Sanfuentes 2357, Santiago, Chile. ABSTRACT. A succession of marine and continental strata on the southern flank of Cerro Cono in the Sierra Baguales, northeast of Torres del Paine, can be correlated with stratigraphic units exposed along the southern border of the Lago Argentino region in Santa Cruz Province, Argentina. -
Figure 6 Outcrop Sections.Cdr
Journal of Sedimentary Research, 2013, v. 83, 746–765 Research Article DOI: 10.2110/jsr.2013.56 ANATOMY AND SEQUENCE ARCHITECTURE OF THE EARLY POST-RIFT IN THE NEUQUE´ N BASIN (ARGENTINA): A RESPONSE TO PHYSIOGRAPHY AND RELATIVE SEA-LEVEL CHANGES 1 1 1 2 GONZALO D. VEIGA, ERNESTO SCHWARZ, LUIS A. SPALLETTI, AND JOSE´ L. MASSAFERRO 1Centro de Investigaciones Geolo´gicas, Universidad Nacional de La Plata-CONICET, Calle 1, #644, B1900TAC, La Plata, Argentina 2YPF S.A. Macacha Gu¨emes 515, C.A. de Buenos Aires, Argentina ABSTRACT: A detailed architectural and sequence stratigraphic analysis was carried out in the early-post-rift succession of central Neuque´n Basin (Middle Jurassic Cuyo Group), integrating outcrop and subsurface information from a 3,000 km2 area. Sedimentary facies analysis allowed the definition of six marine facies associations, which are grouped in two main depositional systems. During the late Toarcian to early Bathonian a storm- and wave-dominated shoreface to offshore system was developed. This is overlain by a late Bathonian–early Callovian fluvio-deltaic depositional system. The sequence stratigraphic analysis of this succession identified parasequences limited by marine flooding surfaces with little evidence of erosion. Parasequences could be grouped into four parasequence sets that show the evolution of the depositional systems and can be interpreted in terms of shoreline trajectories. In this sense, a log-term transgressive event defined by a complicated retrogradational stacking pattern and spanning for almost 10 My is identified for the older deposits. This succession is eventually replaced by a progradational unit that represents highstand conditions. The Cuyo succession identified in this part of the basin is completed by the development of a regressive surface and the onset of a deltaic depositional system with no parasequence development but indicating an abrupt basinward facies shift. -
36490 UT Geofoun NL Rev.P65
John A. and Katherine G. Jackson Geological Sciences Building at Austin The University of Texas Department of Geological Sciences and Geology Foundation 2001 NEWSLETTER 2001 NEWSLETTER The University of Texas at Austin Department of Geological Sciences and Geology Foundation Volume 51 East Mall view of the John A. and Katherine G. Jackson Geological Sciences Building Jackson Building Addition Provides for Expanded State-of-the-Art Instructional and Research Facilities An extraordinary gift from John A. and Katherine G. Jackson will fund a new 57,000 gross-square-foot addition to the present Geology Building. The new complex, consisting of the current building and the new addition, will be named the John A. and Katherine G. Jackson Geological Sciences Building in honor of the donors. As a defining element on the East Mall of the main campus, the building addition will have an exterior design that conforms to the traditional guidelines of the Campus Master Plan while gracefully complementing the shellstone cladding on the exterior of the present building (see covers). A bottom story of cut limestone will underlie three stories of brick with window arrangements echoing those found on the present building. The top story will be limestone with large glass windows under a red tile roof. Interior finishes will highlight natural colors and textures: terrazzo flooring and natural limestone and granite will be set into color schemes centered on a variety of earth tones. Four general-purpose classrooms and three specialized laboratory classrooms will be the focus of instructional activities in the building. The larger general-purpose classrooms all use a tiered or slanted seating arrangement to optimize sight lines to the instructor, and all have been designed to incorporate the latest in instructional technology—dual rear- projection digital display systems. -
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. -
Structural Restoration and Basin and Petroleum Systems Modeling
Structural Restoration and Basin and Petroleum Systems Modeling: Case Studies from the Monagas Fold and Thrust Belt, Venezuela and the Moroccan Atlantic Margin Von der Fakultät für Georessourcen und Materialtechnik der Rheinisch -Westfälischen Technischen Hochschule Aachen zur Erlangung des akademischen Grades eines Doktors der Naturwissenschaften genehmigte Dissertation vorgelegt von Martin Neumaier, MSc aus Freiburg im Breisgau, Deutschland Berichter: Univ.-Prof. Dr. rer. nat. Ralf Littke Univ.-Prof. Peter A. Kukla, Ph.D. Tag der mündlichen Prüfung: 24.04.2015 Diese Dissertation ist auf den Internetseiten der Hochschulbibliothek online verfügbar Abstract This thesis proposes a workflow of integrating structural restoration and basin and petroleum systems modeling. It describes advantages and limitations, and its practical application in structurally complex geological environments dominated by tectonic compression and salt tectonics. The first part of the thesis (chapter 1) presents a study of the Monagas Fold and Thrust Belt onshore northern Venezuela and its deformed foreland basin. The chapter presents for the first time a two-dimensional structural restoration in combination with full PVT three-phase hydrocarbon migration modeling in the study area. The model contributes to the further understanding of the evolution of petroleum systems in fold and thrust belts in general and increases the knowledge of the study area in particular, as it explains the hydrocarbon charge of the main known fields and the relative absence of charge in other areas. In a more theoretical part, the study challenges the simple backstripping approach by applying the structural restoration technique for improved petroleum systems modeling. Particular attention is paid to the decompaction and compaction limitations and its implications for the modeling results. -
The Guiana Shield
THIRTEEN The Guiana Shield NATHAN K. LUJAN and JONATHAN W. ARMBRUSTER Highland areas that serve as sources and boundaries for the a superfamily sister to all other Siluriformes, and their bio- great rivers of South America can be broadly divided into two geographic tractability due to distributions across headwater categories based on their geologic age and origin. As reviewed habitats and associated allopatric distribution patterns among elsewhere in this volume (Chapters 15 and 16), the allochtho- sister taxa. We conclude that the diverse loricariid fauna of the nous terrains and massive crustal deformations of the Andes Guiana Shield accumulated gradually over tens of millions of Mountains that comprise the extremely high-elevation west- years with major lineages being shaped by geologic evolution ern margin of South America have their origins in diastrophic across the whole continent, and not as the result of a rapid, (distortional) tectonic activity largely limited to the Late Paleo- geographically restricted adaptive radiation. We demonstrate gene and Neogene (<25 Ma; Gregory-Wodzicki 2000). In con- the role of the Guiana and Brazilian shields as ancient reser- trast, vast upland regions across much of the interior of the voirs of high-gradient lotic habitats infl uencing the origin of continent have been relatively tectonically quiescent since the frequently rheophilic loricariid taxa. We also show how diver- Proterozoic (>550 Ma; Gibbs and Baron 1993) and exhibit a sifi cation was infl uenced by a restricted number of landscape topography that is instead largely the result of nondeforma- scale features: especially dispersal and vicariance across several tional, epeirogenic uplift of the Guiana and Brazilian shields geologically persistent corridors, expansion and contraction of and subsequent erosion of overlying sedimentary formations.