John Kingston1 Open-File Report 94-559 This Report Is Preliminary and Has Not Been Reviewed for Conformity with U.S. Geological

Total Page:16

File Type:pdf, Size:1020Kb

John Kingston1 Open-File Report 94-559 This Report Is Preliminary and Has Not Been Reviewed for Conformity with U.S. Geological U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY UNDISCOVERED PETROLEUM OF SOUTHERN SOUTH AMERICA by John Kingston1 Open-File Report 94-559 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1 Palo Alto f CA (retired) Table of Contents Undiscovered Petroleum of Southern South America Page List of Figures ..............................................iii List of Tables ............................................xvii Abstract ............................................... 1 I. Introduction ............................................... 1 A. Regions of Study ...................................... 1 B. Purpose and Method of Study ........................... 1 II. Brazilian Craton Region ................................... 4 A. The Rifted Continental Margin Basins .................. 7 1. General .......................................... 7 2. Individual Basin Assessment ...................... 16 a. Southern Rifted Continental Margins .......... 16 1) Campos ................................... 16 2) Santos ................................... 53 3) Pelotas .................................. 59 4) Espirito Santo............................ 63 5) Bahia Sul................................. 74 6) Sergipe-Alagoas........................... 79 b. Northeastern Rifted and Wrenched Margin ...... 89 1) Potiguar.................................. 92 2) Caera.................................... 101 3) Barreirinhas............................. 109 4) Para-Maranhoa............................ 117 5) Foz do Amazonas.......................... 123 6) Guyana................................... 132 B. Brazilian Interior Rift Basins ...................... 138 1. Recancavo ....................................... 138 2. Tucano and Jatoba ............................... 144 3. Tacutu .......................................... 152 C. Brazilian Interior Sag Basins ....................... 157 1. Solimoes ........................................ 158 2. Amazonas ........................................ 168 3. Parnaiba ........................................ 175 4. Parana .......................................... 186 5. Chaco ........................................... 194 D. Subandian Foreland ................................. 194 1. Acre ............................................ 194 III. Patagonian Accreted Region ............................. 201 A. Foreland/Interior Rift Basins ....................... 201 1. Magallanes ..................................... 203 2. Malvinas ........................................ 212 3. Malvinas Plateau ................................ 218 4. Malvinas Trough ................................. 221 5. San Jorge ....................................... 223 6. Colorado ........................................ 234 7. Salado .......................................... 239 8. Nirihuah ........................................ 244 9. Neuquen ......................................... 244 10. Cuyo.............................................253 B. Rifted Continental Margin Basin ..................... 260 1. East Patagonia .................................. 260 IV. Subandian Basins ........................................ 267 A. Foreland Basins ..................................... 269 1. Pampeanas ...................................... 270 2. Oran ............................................ 274 3. Santa Cruz-Tarija ............................... 284 4. Beni ............................................ 294 5. Madre de Dios ................................... 300 6. Ucayali ......................................... 304 7. Maranon-Oriente-Putumayo ........................ 314 B. Overthrust and Fold Belt Basins ..................... 329 1. Huallaga ........................................ 329 2. Santiago ........................................ 336 C. Andean Intra-Arc Basin .............................. 338 1. Altiplano ....................................... 339 D. Pacific Coastal Forearc and Intra-arc Basins ........ 344 1. Puruvian and Ecuadorian Coastal Basins ..........344 a. Forearc Basins .............................. 345 1) Talara...................................348 2) Progreso................................. 355 3) Esmeraldas-Caraguez...................... 363 4) Trujillo................................. 366 5) Lima..................................... 371 6) Mellenda-Tarapaca........................ 371 b. Intra-arc Basins ............................ 374 1) Lancones................................. 374 2) Manibi...................................376 3) Borbon...................................378 4) Sechura.................................. 380 5) Salaverry................................ 383 6) Pisco.................................... 386 7) Moquegua-Tamaruga........................ 390 8) Salar de Atacama (Antofagasta)........... 392 2. South Chilean Coastal Basins .................... 393 a. Forearc Basins .............................. 393 1) Central Chilean ......................... 395 2) Madre de Dios............................ 403 3) Diego Ramirez............................ 406 b. Coastal Intra-arc Basins .................... 409 1) Osorno-Llanguehue........................ 409 2) Temuco................................... 411 3) Carico...................................412 4) Penas.................................... 413 V. Summary and Conclusions .................................. 415 Bibliography ............................................. 428 Appendix A ............................................. 438 11 List of Figures Page 1. Map showing the five principal geotectonic regions of South America. ................................. 3 2. Map showing principal sedimentary basins of the Brazilian Shield area. .................................... 5 3. Map of the Brazilian Atlantic margin. ..................... 9 4. Structure map on top of acoustic basement in the Campos basin. ............................................ 10 5. Section showing tecto-sedimentary evolution of the Brazilian continental margin in the Campos basin. ........ 12 6. Geologic strike section through the Brazilian rifted continental marginal basins. ...................... 14 7. Index map of the Campos basin. ........................... 18 8. Stratigraphic column of Campos basin shelf. .............. 19 9. Geochemical profiles of various parameters as observed in through the oil-generating zone of Wildcat R-JS-76 of central Campos basin. ................. 21 10. Subsidence rates along the Brazilian continental margin. .................................................. 23 11. Campos basin oil fields and production systems, 1988. .................................................... 26 12. Graph showing the relation of the quantity of discovered oil and gas against the number of wildcat drilled in the Campos basin. ..................... 28 13. Structural-stratigraphic section through the Badejo high of the Campos basin. ......................... 31 14. Dip seismic section through the Campos basin. ............ 34 15. Isopach maps of Cretaceous combined sandstone thicknesses, in meters, on the Campos basin shelf. ....... 35 16. Stratigraphic column of the Tertiary section of the Albacora Field of the Campos basin. .................. 37 17. Paleogeography of the Oligocene turbidite system in Campos basin. ......................................... 38 111 18. Location map of the Albacora and Marlim fields and 3-D surveys in deep water (modified from Souza et al, 1989). ............................................ 40 19. A 3-D seismic dip section across the Albacora Field and its interpretation. .................................. 41 20. Seismic profiles (A and B) across the Marlin and Barracuda complex of fields. ............................ 42 21. A 3-D seismic strike section through the Marlim field showing its interpretation and the anomalously high reflection amplitude at the top interface of an oil-filled Eocene turbidite. ............................. 43 22. Maps of the Marlim-Barracuda field complexes showing how clearly the fields, particularly the Marlim complex, are outlined by high amplitude effects at the top of the main Oligocene turbidites. ..... 44 23. Map showing prospective deep-water areas of the Campos basin being considered for future drilling. ....... 46 24. Seismic section A-A' indicating eastward extension of reservoirs (cross-hatched) of Campos basin identified in wildcat l-RJS-366 and independent structure to southeast. .................................. 47 25. Seismic section B-B' in the Albacora area showing reservoirs (cross-hatched) of Campos basin and emphasizing synrift targets. ............................. 48 26. Seismic section C-C' in wildcat l-RJS-490 area of Campos basin showing interpreted reservoirs (cross-hatched) including possible (OLIG) Oligocene lowstand fan system. ........................... 49 27. Seismic section D-D at extreme south of Campos basin showing complex structure and in particular faults which cut Miocene reservoir horizons (cross-hatched) and may serve as conduits for oil migration. ........................................... 50 28. Index map of the Santos basin showing position of gas and oil fields, geologic sections and wildcats. ...... 54 29. Stratigraphic chart of Santos basin. ..................... 55 30. Geologic section in southern portion of Santos basin. ................................................... 56 31. Geologic section of central portion of Santos basin. ....
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Structural Modeling Based on Sequential Restoration of Gravitational Salt Deformation in the Santos Basin (Brazil)
    Marine and Petroleum Geology xxx (2012) 1e17 Contents lists available at SciVerse ScienceDirect Marine and Petroleum Geology journal homepage: www.elsevier.com/locate/marpetgeo Structural modeling based on sequential restoration of gravitational salt deformation in the Santos Basin (Brazil) Sávio Francis de Melo Garcia a,*, Jean Letouzey b, Jean-Luc Rudkiewicz b, André Danderfer Filho c, Dominique Frizon de Lamotte d a Petrobras E&P-EXP, Rio de Janeiro, Brazil b IFP Energies Nouvelles, France c Universidade Federal de Ouro Preto, Ouro Preto/MG, Brazil d Université de Cergy-Pontoise, France article info abstract Article history: The structural restoration of two parallel cross-sections in the central portion of the Santos Basin enables Received 8 December 2010 a first understanding of existent 3D geological complexities. Santos Basin is one of the most proliferous Received in revised form basins along the South Atlantic Brazilian margin. Due to the halokinesis, geological structures present 22 November 2011 significant horizontal tectonic transport. The two geological cross-sections extend from the continental shelf Accepted 2 February 2012 to deep waters, in areas where salt tectonics is simple enough to be solved by 2D restoration. Such cross- Available online xxx sections display both extensional and compressional deformation. Paleobathymetry, isostatic regional compensation, salt volume control and overall aspects related to structural style were used to constrain basic Keywords: fl Salt tectonics boundary conditions. Several restoration
    [Show full text]
  • Basement Composition and Basin Geometry Controls on Upper-Crustal Deformation in the Southern Central Andes (30–36° S)
    Geol. Mag.: page 1 of 17 c Cambridge University Press 2016 1 doi:10.1017/S0016756816000364 Basement composition and basin geometry controls on upper-crustal deformation in the Southern Central Andes (30–36° S) ∗ ∗ ∗ JOSÉ F. MESCUA †, LAURA GIAMBIAGI , MATÍAS BARRIONUEVO , ∗ ∗ ANDRÉS TASSARA‡, DIEGO MARDONEZ , MANUELA MAZZITELLI ∗ & ANA LOSSADA ∗ Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), Centro Científico Tecnológico Mendoza, CONICET. Av. Ruiz leal s/n Parque General San Martín, Mendoza (5500) Argentina ‡Departamento de Ciencias de la Tierra, Universidad de Concepción, Victor Lamas 1290, Barrio Universitario, Concepción, Casilla 160-C, Chile (Received 13 December 2015; accepted 5 April 2016) Abstract – Deformation and uplift in the Andes are a result of the subduction of the Nazca plate below South America. The deformation shows variations in structural style and shortening along and across the strike of the orogen, as a result of the dynamics of the subduction system and the features of the upper plate. In this work, we analyse the development of thin-skinned and thick-skinned fold and thrust belts in the Southern Central Andes (30–36° S). The pre-Andean history of the area determined the formation of different basement domains with distinct lithological compositions, as a result of terrane accretions during Palaeozoic time, the development of a widespread Permo-Triassic magmatic province and long-lasting arc activity. Basin development during Palaeozoic and Mesozoic times produced thick sedimentary successions in different parts of the study area. Based on estimations of strength for the different basement and sedimentary rocks, calculated using geophysical estimates of rock physical properties, we propose that the contrast in strength between basement and cover is the main control on structural style (thin- v.
    [Show full text]
  • Plateau-Style Accumulation of Deformation: Southern Altiplano
    TECTONICS, VOL. 24, TC4020, doi:10.1029/2004TC001675, 2005 Plateau-style accumulation of deformation: Southern Altiplano Kirsten Elger, Onno Oncken, and Johannes Glodny GeoForschungsZentrum Potsdam, Potsdam, Germany Received 5 May 2004; revised 17 December 2004; accepted 23 March 2005; published 31 August 2005. [1] Employing surface mapping of syntectonic during the Paleogene, initially reactivating crustal sediments, interpretation of industry reflection- weak zones and by thermal weakening of the crust seismic profiles, gravity data, and isotopic age dating, with active magmatism mainly in the Neogene stage. we reconstruct the tectonic evolution of the southern Citation: Elger, K., O. Oncken, and J. Glodny (2005), Plateau- Altiplano (20–22°S) between the cordilleras style accumulation of deformation: Southern Altiplano, Tectonics, defining its margins. The southern Altiplano crust 24, TC4020, doi:10.1029/2004TC001675. was deformed between the late Oligocene and the late Miocene with two main shortening stages in the Oligocene (33–27 Ma) and middle/late Miocene 1. Introduction (19–8 Ma) that succeeded Eocene onset of shortening at the protoplateau margins. Shortening [2] Although considerable advance has been made in recent years in understanding the processes involved in rates in the southern Altiplano ranged between 1 and the formation of orogenic plateaus, the precise temporal 4.7 mm/yr with maximum rates in the late Miocene. and spatial patterns of uplift and lateral progradation of Summing rates for the southern Altiplano and the
    [Show full text]
  • Lacustrine Coquinas and Hybrid Deposits from Rift Phase Pre-Salt
    Journal of South American Earth Sciences 95 (2019) 102254 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Lacustrine coquinas and hybrid deposits from rift phase: Pre-Salt, lower T Cretaceous, Campos Basin, Brazil Vinicius Carbone Bernardes de Oliveiraa,b,*, Carlos Manuel de Assis Silvaa, Leonardo Fonseca Borghib, Ismar de Souza Carvalhob a Petrobras Research and Development Center (CENPES), Avenida Horacio de Macedo, 950, Ilha do Fundao – Cidade Universitaria, Rio de Janeiro, RJ, 21949-915, Brazil b Universidade Federal do Rio de Janeiro, Centro de Ciencias Matematicas e da Natureza, Instituto de Geociencias, Departamento de Geologia, Programa de Pos-graduacao em Geologia, Av. Athos da Silveira Ramos, 274, Bloco F, Ilha do Fundao – Cidade Universitaria, Rio de Janeiro, RJ, 21949-900, Brazil ARTICLE INFO ABSTRACT Keywords: This study presents a facies characterization, facies succession and conceptual depositional model of the Pre-salt Coqueiros Formation, Lower Cretaceous of Campos Basin, based on core analyses of two wells. WELL-1 is a Rift sedimentation shallow water drilling located at south of Campos Basin within the Badejo structural high, and WELL-2 is an ultra Coquinas deep water drilling located at north, over the “External High”. Ten carbonate facies, three siliciclastic facies, two Hybrid deposits magnesium clay mineral rich facies and two hybrid facies were identified. The carbonate facies were defined as Lower cretaceous rudstone, grainstone, packstone and mud supported carbonate rock, composed of bivalves, ostracods, and rare gastropods. Bivalve shells, mostly disarticulated with distinct degrees of fragmentation, characterized the main components of the ten carbonate facies.
    [Show full text]
  • IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment
    IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment IV. NORTHERN SOUTH AMERICA SUMMARY Northern South America has prospective shale gas and shale oil potential within marine- deposited Cretaceous shale formations in three main basins: the Middle Magdalena Valley and Llanos basins of Colombia, and the Maracaibo/Catatumbo basins of Venezuela and Colombia, Figure IV-1. The organic-rich Cretaceous shales (La Luna, Capacho, and Gacheta) sourced much of the conventional gas and oil produced in Colombia and western Venezuela, and are similar in age to the Eagle Ford and Niobrara shale plays in the USA. Ecopetrol, ConocoPhillips, ExxonMobil, Shell, and others have initiated shale exploration in Colombia. Colombia’s petroleum fiscal regime is considered attractive to foreign investment. Figure IV-1: Prospective Shale Basins of Northern South America Source: ARI 2013 May 17, 2013 IV-1 IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment For the current EIA/ARI assessment, the Maracaibo-Catatumbo Basin was re-evaluated while new shale resource assessments were undertaken on the Middle Magdalena Valley and Llanos basins. Technically recoverable resources (TRR) of shale gas and shale oil in northern South America are estimated at approximately 222 Tcf and 20.2 billion bbl, Tables IV-1 and IV- 2. Colombia accounts for 6.8 billion barrels and 55 Tcf of risked TRR, while western Venezuela has 13.4 billion barrels and 167 Tcf. Eastern Venezuela may have additional potential but was not assessed due to lack of data. Colombia’s first publicly disclosed shale well logged 230 ft of over-pressured La Luna shale with average 14% porosity.
    [Show full text]
  • 40. Geologic History and Origin of Sao Paulo
    40. GEOLOGIC HISTORY AND ORIGIN OF SAO PAULO PLATEAU (SOUTHEASTERN BRAZILIAN MARGIN), COMPARISON WITH THE ANGOLAN MARGIN, AND THE EARLY EVOLUTION OF THE NORTHERN SOUTH ATLANTIC Naresh Kumar and L.A.P. Gamboa,1 Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York B.C. Schreiber, Queens College, City University of New York, Flushing, New York and J. Mascle, Université Pierre et Marie Curie, Centre de Geodynamique sous Marine, 06230 Villefranche - sur mer, France ABSTRACT The Sào Paulo Plateau is a prominent marginal plateau in the southern Brazilian margin. It is underlain by oceanic crust and is bounded to the north and south by fracture zones. Seismic profiles and drilling data from Site 356 (located on its southeastern corner) indicate that the region occupied by the plateau has acted as a depocenter and has evolved as a marginal plateau since the Aptian time. The Oceanographic conditions and depositional environments prevailing over the plateau during its early evolution were almost identical to those suggested in the Angolan margin by the drilling data at Site 364 (DSDP). Reconstruction of the evolution of Sào Paulo Plateau and com- parison between the drilled geologic sequences on the opposing margins suggest the following history for the northern South Atlan- tic. Coarse terrigenous sediments were deposited in coastal basins at both the margins following the opening of the South Atlantic in the Neocomian. By Aptian time, a linear narrow basin, with barriers to the south and north, was created. The Walvis and Sào Paulo ridges formed the southern barrier whereas the equatorial fracture zones appear to have formed the northern barrier.
    [Show full text]
  • A Revised Position for the Rotated Falkland Islands Microplate
    1 A revised position for the rotated Falkland Islands microplate 2 Roxana M. Stanca1*, Douglas A. Paton1, David M. Hodgson1, Dave J. McCarthy2 & Estelle J. 3 Mortimer1 4 1School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom 5 2Lyell Centre, British Geological Survey, Edinburgh EH14 4AP, United Kingdom 6 *Corresponding author (e-mail: [email protected]) 7 ABSTRACT: The early stages of transform margin formation are associated with crustal 8 fragmentation and block rotation. The restricted size of the resultant microcontinental blocks 9 precludes palaeogeographic reconstructions and reliable estimations of the amount of rotation 10 they can undergo. An example considered here is the Falkland Plateau. This is located adjacent to 11 the Agulhas-Falkland Fracture Zone/Transform and its westernmost province is the Falkland 12 Islands microcontinent. The position of the plateau and the islands prior to Gondwana break-up 13 remains contentious. This study integrates seismic reflection and gravity data to propose a 14 revised position of the Falkland Islands microcontinent constrained by: (a) the presence of a 15 mega-décollement, controlling the Gondwanide Orogen, described north of the Falkland Islands 16 and underneath South Africa and Outeniqua Basin, and (b) the similar architecture of fault 17 networks mapped north of the islands and in the northernmost Outeniqua Basin. This revised 18 position requires a re-evaluation of the timing and rate of rotation of the Falkland Islands 19 microcontinent and impacts the expected crustal architecture adjacent to the islands. Our model 20 yields rotation rates between 5.5° and 8° Myr-1, two potential times for rotation and predicts more 21 unstretched crust beneath the basin east of the Falkland Islands than previous models.
    [Show full text]
  • Detrital Zircon Record of Phanerozoic Magmatism in the Southern Central Andes GEOSPHERE, V
    Research Paper GEOSPHERE Detrital zircon record of Phanerozoic magmatism in the southern Central Andes GEOSPHERE, v. 17, no. 3 T.N. Capaldi1,*, N.R. McKenzie2, B.K. Horton1,3, C. Mackaman-Lofland1, C.L. Colleps2, and D.F. Stockli1 1Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78712, USA https://doi.org/10.1130/GES02346.1 2Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong, China 3Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78712, USA 11 figures; 1 table; 1 set of supplemental files CORRESPONDENCE: [email protected] ABSTRACT arc width reflects shallower slab dip. Comparisons geodynamic processes, upper-plate deformation, among slab dip calculations with time-averaged and subduction- related magmatism. CITATION: Capaldi, T.N., McKenzie, N.R., Horton, B.K., Mackaman-Lofland, C., Colleps, C.L., and Stockli, D.F., The spatial and temporal distribution of arc εHf and Th/U zircon results exhibit a clear trend of The South American plate at 28°S –33°S is com- 2021, Detrital zircon record of Phanerozoic magmatism magmatism and associated isotopic variations decreasing (enriched) magma compositions with posed of numerous north-south–trending terranes in the southern Central Andes: Geosphere, v. 17, no. 3, provide insights into the Phanerozoic history increasing arc width and decreasing slab dip. Col- of variable composition that may have induced a p. 876– 897, https://doi.org/10.1130 /GES02346.1. of the western margin of South America during lectively, these data sets demonstrate the influence spatial control on the geochemical signatures of Science Editor: Shanaka de Silva major shifts in Andean and pre-Andean plate inter- of subduction angle on the position of upper-plate subsequent Andean tectono-magmatic regimes Associate Editor: Christopher J.
    [Show full text]
  • Geotectonic Controls on CO2 Formation and Distribution Processes in the Brazilian Pre-Salt Basins
    geosciences Article Geotectonic Controls on CO2 Formation and Distribution Processes in the Brazilian Pre-Salt Basins Luiz Gamboa 1,*, André Ferraz 1, Rui Baptista 2 and Eugênio V. Santos Neto 3 1 Geology & Geophysical Department, Universidade Federal Fluminense, UFF, Niterói 2410-364, Brazil; [email protected] 2 Geology Department, F. Ciências Universidade de Lisboa, 1749-016 Lisboa, Portugal; [email protected] 3 Independent Consultant, Rio de Janeiro 22271-110, Brazil; [email protected] * Correspondence: [email protected] Received: 7 March 2019; Accepted: 16 May 2019; Published: 5 June 2019 Abstract: Exploratory work for hydrocarbons along the southeastern Brazilian Margin discovered high concentrations of CO2 in several fields, setting scientific challenges to understand these accumulations. Despite significant progress in understanding the consequences of high CO2 in these reservoirs, the role of several variables that may control such accumulations of CO2 is still unclear. For example, significant differences in the percentages of CO2 have been found in reservoirs of otherwise similar prospects lying close to each other. In this paper, we present a hypothesis on how the rifting geodynamics are related to these CO2-rich accumulations. CO2-rich mantle material may be intruded into the upper crustal levels through hyper-stretched continental crust during rifting. Gravimetric and magnetic potential methods were used to identify major intrusive bodies, crustal thinning and other geotectonic elements of the southeastern Brazilian Margin. Modeling based on magnetic, gravity, and seismic data suggests a major intrusive magmatic body just below the reservoir where a high CO2 accumulation was found. Small faults connecting this magmatic body with the sedimentary section could be the fairway for the magmatic sourced gas rise to reservoirs.
    [Show full text]
  • A Review of Tertiary Climate Changes in Southern South America and the Antarctic Peninsula. Part 1: Oceanic Conditions
    Sedimentary Geology 247–248 (2012) 1–20 Contents lists available at SciVerse ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Review A review of Tertiary climate changes in southern South America and the Antarctic Peninsula. Part 1: Oceanic conditions J.P. Le Roux Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile/Centro de Excelencia en Geotérmia de los Andes, Casilla 13518, Correo 21, Santiago, Chile article info abstract Article history: Oceanic conditions around southern South America and the Antarctic Peninsula have a major influence on cli- Received 11 July 2011 mate patterns in these subcontinents. During the Tertiary, changes in ocean water temperatures and currents Received in revised form 23 December 2011 also strongly affected the continental climates and seem to have been controlled in turn by global tectonic Accepted 24 December 2011 events and sea-level changes. During periods of accelerated sea-floor spreading, an increase in the mid- Available online 3 January 2012 ocean ridge volumes and the outpouring of basaltic lavas caused a rise in sea-level and mean ocean temper- ature, accompanied by the large-scale release of CO . The precursor of the South Equatorial Current would Keywords: 2 fi Climate change have crossed the East Paci c Rise twice before reaching the coast of southern South America, thus heating Tertiary up considerably during periods of ridge activity. The absence of the Antarctic Circumpolar Current before South America the opening of the Drake Passage suggests that the current flowing north along the present western seaboard Antarctic Peninsula of southern South American could have been temperate even during periods of ridge inactivity, which might Continental drift explain the generally warm temperatures recorded in the Southeast Pacific from the early Oligocene to mid- Ocean circulation dle Miocene.
    [Show full text]