Vaca Muerta: from Source to Reservoir
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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 -
Bivalvia, Late Jurassic) from South America
Author's personal copy Pala¨ontol Z DOI 10.1007/s12542-016-0310-z RESEARCH PAPER Huncalotis, an enigmatic new pectinoid genus (Bivalvia, Late Jurassic) from South America 1 2 Susana E. Damborenea • He´ctor A. Leanza Received: 29 September 2015 / Accepted: 16 March 2016 Ó Pala¨ontologische Gesellschaft 2016 Abstract The extensive outcrops of the Late Jurassic– orientated at right angles to the shell margins. A few speci- Early Cretaceous Vaca Muerta Formation black shales and mens were found on the outside of large calcareous con- marls in the Neuque´n Basin have yielded very few bivalves, cretions within black shales; these are often articulated, and these are not well known. The material described here complete shells, which preserve the original convexity of the was collected in central Neuque´n, from late Tithonian cal- valves. In some cases these articulated shells seem to be careous levels within the black shales, between beds with associated with large ammonite shells, suggesting an epi- Substeueroceras sp. and with Argentiniceras noduliferum byssate (possibly also pseudoplanktonic) lifestyle. (Steuer). The material is referred to the new genus Huncalotis and to the new species H. millaini. The strongly Keywords Late Tithonian Á Neuque´n Basin Á Vaca inequivalve shells, the ligamental area with a triangular Muerta Formation Á Argentina Á Peru Á Bivalvia Á slightly prosocline resilifer, the right valve with ctenolium Pectinoidea Á Pectinidae and a very deep byssal notch, and the lack of radial orna- mentation make the shell of this new genus strikingly similar Kurzfassung Die reichlich zutage tretenden Schwarz- to the Triassic pectinid Pleuronectites. -
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. -
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. -
This Manuscript Is a Preprint and Has Been Formally Accepted for Publication in Basin Research
This manuscript is a preprint and has been formally accepted for publication in Basin Research 1 Base-Salt Relief Controls on Salt-Tectonic Structural Style, São Paulo Plateau, Santos Basin, Brazil *Leonardo M. Pichel1, Christopher A-L. Jackson1; Frank Peel1,2, Tim P. Dooley2 1 – Basins Research Group (BRG), Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, SW7 2BP, United Kingdom 2 – The University of Texas at Austin, Bureau of Economic Geology, Jackson School of Geosciences, Austin, Texas, USA Key-words: SALT TECTONICS, MINIBASINS, DIAPIRISM, TRANSLATION, BASE- SALT RELIEF, RAMP-SYNCLINE BASINS, GRAVITY-DRIVEN DEFORMATION, SANTOS BASIN, BRAZIL, SÃO PAULO PLATEAU 2 ABSTRACT Base-salt relief influences salt flow, producing three-dimensionally complex strains and multiphase deformation within the salt and its overburden. Understanding how base-salt relief influences salt-related deformation is important to correctly interpret salt basin kinematics and distribution of structural domains, which have important implications to understand the development of key petroleum system elements. The São Paulo Plateau, Santos Basin, Brazil is characterized by a >2 km thick, mechanically layered Aptian salt layer deposited above prominent base-salt relief. We use 3D seismic reflection data, and physical and conceptual kinematic models to investigate how gravity-driven translation above thick salt, underlain by complex base-salt relief, generated a complex framework of salt structures and minibasins. We show that ramp-syncline basins developed above and downdip of the main pre- salt highs record c. 30 km of Late Cretaceous-Paleocene basinward translation. As salt and overburden translated downdip, salt flux variations caused by the base-salt relief resulted in non-uniform motion of the cover, and the simultaneous development of extensional and contractional structures. -
Porosity Permeability Volume and Lifespan Gabriel Wimmerth
POROSITY PERMEABILITY VOLUME AND LIFESPAN GABRIEL WIMMERTH 1 THE POROSITY OF A RESERVOIR DETERMINES THE QUANTITY OF OIL AND GAS. THE MORE PORES A RESERVOIR CONTAINS THE MORE QUANTITY, VOLUME OF OIL AND GAS IS PRESENT IN A RESERVOIR. BY GABRIEL KEAFAS KUKU PLAYER WIMMERTH DISSERTATION PRESENTED FOR THE DEGREE OF DOCTORATE IN PETROLEUM ENGINEERING In the Department of Engineering and Science at the Atlantic International University, Hawaii, Honolulu, UNITED STATES OF AMERICA Promoter: Dr. Franklin Valcin President/Academic Dean at Atlantic International University October 2015 2 DECLARATION I declare by submitting this thesis, dissertation electronically that that the comprehensive, detailed and the entire piece of work is my own, original work that I am the sole owner of the copyright thereof(unless to the extent otherwise stated) and that I have not previously submitted any part of the work in obtaining any other qualification. Signature: Date: 10 October 2015 Copyright@2015 Atlantic International University All rights reserved 3 DEDICATION This work is dedicated to my wife Edla Kaiyo Wimmerth for assisting, encouraging, motivating and being a strong pillar over the years as I was completing this dissertation. It has been quite a tremendous journey, hard work and commitment for me and I would not have completed this enormous work, dissertation without her weighty, profound assistance. 4 ABSTRACT The oil and gas industry, petroleum engineering, exploration, drilling, reservoir and production engineering have taken an enormous toll since the early forties and sixties and it has predominantly reached the peak in the early eighties and nineties. The number of oil and gas companies have been using the vertical drilling approach and successfully managed to pinch the reservoir with productive oil or gas. -
Tetrápodos Jurásico-Cretácicos
TETRÁPODOS JURÁSICO-CRETÁCICOS Asociación Paleontológica Argentina. Publicación Especial 11 ISSN 0328-347X Ameghiniana 50º aniversario: 125-136. Buenos Aires, 25-11-2007 Reptiles marinos jurásicos y cretácicos de la Patagonia argentina: su aporte al conocimiento de la herpetofauna mesozoica Zulma GASPARINI*, Marta FERNÁNDEZ, Marcelo de la FUENTE y Leonardo SALGADO Abstract. The history of the knowledge of the different groups of Mesozoic marine reptiles of Patagonia can be divided into two major periods: the first one from the end of the XIX century up to 1940, during which the findings were scarce and few taxa are currently valid. The second, from the 1940’s to date. The biogeographic patterns of the marine reptiles during most of the Mesozoic could be analysed on the basis of systematic studies of the Patagonian records. One of the most outstanding paleogeographic events of the Jurassic was the dismembering of Pangea, which gave place to the Caribbean Corridor connecting, probably intermittently, the Western Tethys with the Eastern Pacific. The close affinities between the Jurassic marine reptiles of Argentina and Chile with those of Europe suggest that such corridor would have been one of the routes used by the marine reptiles for their dispersion. Thus, the middle Jurassic forms of Patagonia and Chile belong to genera recorded also in Europe (Metriorhynchus, Stenopterygius, cf. Muraenosarus and cf. Cryptoclidus), or to taxa with close phylogenetic relationships (Maresaurus, Mollesaurus). This is also seen in most of the genera of the Late Jurassic (Ophthalmosaurus, Aegirosaurus, Metriorhynchus, Geosaurus, Dakosaurus, Liopleurodon, Pliosaurus). Likewise, the finding of plesiosaurs and mosasaurs of the end of the Cretaceous in Patagonia arose a new context for the discussion of the biogeo- graphic, distribution of these predators in Southern Gondwana. -
Vaca Muerta Shale Basin Argentina
Vaca Muerta Shale Basin Argentina Sectors: Oil and Gas Extraction, Pipeline Transportation of Crude Oil, Pipeline Transportation of Natural Gas Active This profile is actively maintained Send feedback on this profile By: BankTrack Created on: Feb 17 2020 Last update: Jan 12 2021 Contact: [email protected] Project website Status Planning Design Agreement Construction Operation Closure Decommission Sectors Oil and Gas Extraction, Pipeline Transportation of Crude Oil, Pipeline Transportation of Natural Gas Location Status Planning Design Agreement Construction Operation Closure Decommission Website https://www.ypf.com/Vacamuertachallenge/Paginas/index.html About Vaca Muerta Shale Basin According to the US Energy Information Agency, Argentina has the second-largest shale gas reserves and fourth-largest shale oil reserves in the world. The country's shale gas reserves alone would account for 11.4% of the world’s remaining 1.5°C carbon budget if exploited to its maximum. Nearly all of these reserves are located in the Neuquén Basin in Northern Patagonia. The Vaca Muerta Shale Basin is located in the Neuquén Basin. It has been identified as the largest shale play outside North America. The megaproject entails extraction from the area’s enormous shale oil and gas reserves, as well as building associated infrastructure such as pipelines and LNG terminals. The deposit extends over 30,000 square kilometres and represents 43% of Argentina's total oil production and 60% of its gas production. Initially, this basin was supposed to contribute towards energy self-sufficiency, but recently, the export potential of the region has been realised and more attention is being paid towards exports. -
Watershed Implications of Shale Oil and Gas Production in Vaca Muerta, Argentina
Watershed implications of shale oil and gas production in Vaca Muerta, Argentina SEI working paper April 2021 Laura Forni1 Marina Mautner1,3 Angela Lavado4 Kathleen Fitzpatrick Burke2 Romina Diaz Gomez3 1 SEI 2 Stockholm School of Economics 3 University of California, Davis 4 Consultant Stockholm Environment Institute Linnégatan 87D 115 23 Stockholm, Sweden Tel: +46 8 30 80 44 www.sei.org Author contact: Laura Forni [email protected] Editor: Emily Yehle Layout: Richard Clay Cover photo: Extraction of unconventional oil, Vaca Muerta, Argentina © Cristian Martin / Getty This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes, without special permission from the copyright holder(s) provided acknowledgement of the source is made. No use of this publication may be made for resale or other commercial purpose, without the written permission of the copyright holder(s). Copyright © April 2021 by Stockholm Environment Institute Stockholm Environment Institute is an international non-profit research and policy organization that tackles environment and development challenges. We connect science and decision-making to develop solutions for a sustainable future for all. Our approach is highly collaborative: stakeholder involvement is at the heart of our efforts to build capacity, strengthen institutions, and equip partners for the long term. Our work spans climate, water, air, and land-use issues, and integrates evidence and perspectives on governance, the economy, gender and human health. Across our eight centres in Europe, Asia, Africa and the Americas, we engage with policy processes, development action and business practice throughout the world. Acknowledgments: We would like to thank our project partners and the stakeholders who participated in interviews to clarify certain aspects of the literature. -
Seismic Characterization of Carbonate Platforms and Reservoirs: an Introduction and Review
Downloaded from http://sp.lyellcollection.org/ by guest on September 25, 2021 Seismic characterization of carbonate platforms and reservoirs: an introduction and review James Hendry1,2*, Peter Burgess3, David Hunt4, Xavier Janson5 and Valentina Zampetti6 1Iapetus Geoscience Ltd, Unit 7, Watson & Johnson Centre, Mill Road, Greystones, Co. Wicklow, Ireland 2School of Earth Sciences, University College Dublin, Bellfield, Dublin 4, Ireland 3School of Environmental Sciences, University of Liverpool, Brownlow Street, Liverpool L69 3GP, UK 4Equinor, Sandsliveien 90, Sandsli, N-5234, Norway 5Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX 78713, USA 6Shell Global Solutions, Lange Kleiweg 40, 2288 ER Rijswijk, The Netherlands JH, 0000-0002-8448-6057; DH, 0000-0003-1911-9389 *Correspondence: [email protected] Abstract: Improved seismic data quality in the last 10–15 years, innovative use of seismic attribute combina- tions, extraction of geomorphological data and new quantitative techniques have significantly enhanced under- standing of ancient carbonate platforms and processes. 3D data have become a fundamental toolkit for mapping carbonate depositional and diagenetic facies, and associated flow units and barriers, giving a unique perspective on how their relationships changed through time in response to tectonic, oceanographic and climatic forcing. Sophisticated predictions of lithology and porosity are being made from seismic data in reservoirs with good borehole log and core calibration for detailed integration with structural, palaeoenvironmental and sequence stratigraphic interpretations. Geologists can now characterize entire carbonate platform systems and their large-scale evolution in time and space, including systems with few outcrop analogues such as the Lower Cre- taceous Central Atlantic ‘pre-salt’ carbonates. -
Petroleum Systems of the Vaca Muerta (Tithonian) Formation
Petroleum Systems Charged by the Vaca Muerta (Tithonian) Formation: Neuquén Basin, Argentina WAVREK1, D.A., M.E. LARA2, G.A. LAFFITTE3, S. DEL VO3, J.W. COLLISTER1, J.C. QUICK1, R.B. ALLEN1, D.M. JARVIE4 and H.E. HOLLOWELL5 1E.S.R.I., University of Utah, Salt Lake City, UT 2Lagoven S.A., Caracas, Venezuela 3Y.P.F. S.A., Buenos Aires, Argentina 4H.I.&S., Humble, TX 5Westvaco Resources, Summerville, SC Tithonian (Upper Jurassic) source rock sequences are responsible for a significant volume of petroleum reserves on a global basis. This research defines the petroleum systems within the Neuquén basin that are charged from the Tithonian Vaca Muerta Formation; a unit deposited in a low angle ramp setting that is characterized in seismic and geochemical terms to contain three distinct organic facies. The oil types that correlate to the different organic facies are used to define effective migration pathways. The results indicate that the distal condensed sections are volumetrically significant but physical constraints related to hydrocarbon expulsion and migration contribute to decreased system efficiency. In contrast, the hydrocarbon potential of the shelfal condensed sections have less volumetric significance but exhibit higher efficiency due to the shorter distance required for fracture propagation (i.e., related to the expulsion event) and the effective juxtaposition of migration conduits and/or potential reservoirs. For example, expulsion of hydrocarbons into the underlying Kimmeridgian incised valleys along the Añelo Trough provide a regional migration pathway, whereas expulsion from the top of the unit provides a direct charge into sequences interpreted to represent detached lowstand fans. -
Maquetación 1
Año 2015 - Volumen 15(1): 20-30 VOLUMEN TEMÁTICO ISSN 2469-0228 OPHTHALMOSAURIDS (ICHTHYOSAURIA: THUNNOSAURIA): ALPHA TAXONOMY, CLADES AND NAMES MARTA S. FERNÁNDEZ 1, 2 AND LISANDRO CAMPOS 2 1CONICET. 2División Paleontología Vertebrados, Museo de La Plata, Universidad Nacional de La Plata, Paseo del Bosque s/n, B1900FWA La Plata, Argentina. [email protected] ; [email protected] Abstract . Thunnosaurian ichthyosaurs represent the paradigm of reptilian body designed for a pelagic life style. Most derived thunnosaurian, the ophthalmosaurids, have been traditionally considered as members of a declining lineage. New findings and the re-examination of histori - cal collections radically changed our conceptions about them. Opthalmosaurids were ecologically more diverse than previously thought. The past few decades have seen an increase of nominal species spurred by new findings and analyses. A still unresolved problem is that many species are only known by their holotypes. Nevertheless, morphological disparity is a compelling argument for considering them as valid. All recent cladistic analyses of ichthyosaurs recover ophthalmosaurids as a clade. Neither the addition of new information nor the addition of new enti ties resulted in its collapse. On this basis, the assignment of Linnaean rank to this clade (Ophtalmosauridae) is reasonable as it satisfied the primary recommended criteria for taxa naming: monophyly and stability. As the lists of species and genus names are used as input in major data bases for interpreting major turnover and/or extinction patterns, efforts must be focused on clarifying as much as possible the alpha tax onomy. Two major pending issues are the delimitation of Ophthalmosaurus -Baptanodon, and Platypterygius .