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Triassic-Jurassic Rifting: Continental Breakup and the Origin of the Atlantic Ocean and Passive Margins PDF

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Preview Triassic-Jurassic Rifting: Continental Breakup and the Origin of the Atlantic Ocean and Passive Margins

FURTHER TITLES IN THIS SERIES 1. J. AUBOUIN GEOSYNCLINES 2. R.W. VANBEMMELEN GEODYNAMIC MODELS 3. A. SUGIMURA and S. UYEDA ISLAND ARCS 4. A.R. RITSEMA (Editor) THE UPPER MANTLE 5. C. LOMNITZ GLOBAL TECTONICS AND EARTHQUAKE RISK 6. X. LEPICHON, J. FRANCHETEAU and J. BONNIN PLATE TECTONICS 7. R. W. GIRDLER (Editor) EAST AFRICAN RIFTS 8. S.MUELLER (Editor) THE STRUCTURE OF THE EARTH'S CRUST 9. N. PAVONIandR. GREEN (Editors) RECENT CRUSTAL MOVEMENTS 10. S.W. CAREY THE EXPANDING EARTH U.A.M. JOHNSON STYLES OF FOLDING 12. M.H.P.BOTT (Editor) SEDIMENTARY BASINS OF CONTINENTAL MARGINS AND CRATONS 13. C.A. WHITTEN, R. GREEN and B.K. MEADE (Editors) RECENT CRUSTAL MOVEMENTS, 1977 M.N. TOKSÖZ, S.UYEDA andJ. FRANCHETEAU (Editors) OCEANIC RIDGES AND ARCS 15. C.E.KEEN (Editor) CRUSTAL PROPERTIES ACROSS PASSIVE MARGINS 16. P. VYSKOCIL, R. GREEN and H. MÄLZER (Editors) RECENT CRUSTAL MOVEMENTS, 1979 17. J.H. ILLIES (Editor) MECHANISM OF GRABEN FORMATION 18. E.V. ARTYUSHKOV GEODYNAMICS 19. P. MORGAN and B.H. BAKER (Editors) PROCESSES OF CONTINENTAL RIFTING 20. P. VYSKOCIL A.M. WASSEFandR. GREEN (Editors) RECENT CRUSTAL MOVEMENTS, 1982 21.F.-C. WEZEL (Editor) THE ORIGIN OF ARCS Developments in Geotectonics 22 TRIASSIC-JURASSIC RIFTING Continental Breakup and the Origin of the Atlantic Ocean and Passive Margins Part A Edited by W.MANSPEIZER Department of Geological Sciences, Faculty of Arts and Sciences, Rutgers University, Newark, NJ07102, U.S.A. ELSEVIER r^^itfl^fig* Amsterdam — Oxford — New York — Tokyo, 1988 ELSEVIER SCIENCE PUBLISHERS B.V. Sara Burgerhartstraat 25 P.O. Box 211, 1000 AE Amsterdam, The Netherlands Distributors for the United States and Canada: ELSEVIER SCIENCE PUBLISHING COMPANY INC. 655, Avenue of the Americas New York, NY 10010, U.S.A. ISBN 0-444-42903-4 (Vol. 22) ISBN 0-444-41714-1 (Series) © Elsevier Science Publishers B.V., 1988 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior written permission of the publisher, Elsevier Science Publishers B.V./ Physical Sciences & Engineering Division, P.O. Box 330, 1000 AH Amsterdam, The Netherlands. Special regulations for readers in the U.S.A. - This publication has been registered with the Copy- right Clearance Center Inc. (CCC), Salem, Massachusetts. Information can be obtained from the CCC about conditions under which photocopies of parts of this publication may be made in the USA. All other copyright questions, including photocopying outside of the USA, should be referred to the publisher. No responsibility is assumed by the Publisher for any injury and/or damage to persons or property as a matter of products liability, negligence or otherwise, or from any use or operation of any meth- ods, products, instructions or ideas contained in the material herein. Printed in The Netherlands Preface These are extraordinary times for Triassic - Jurassic researchers of the Atlantic passive margins. Extensive field studies on the African and North American plates during this past decade have yielded a wealth of new data and ideas about rift basins and the origin of passive margins, that but a few years ago would have seemed like childish speculation. New surface and subsurface basins have been identified, fossils abound in strata that only recently were considered barren, oil exploration is being pursued actively in continental strata of the Richmond-Taylorsville, Sanford and Newark basins, Late Triassic marine strata have been identified in Georges Bank off the coast of Massachusetts, and the roles of wrench tectonics, successor basins and listric normal faults have challenged the classical view that these are sim- ple extensional basins. This volume brings together representative examples of these studies. It is not meant to be an exhaustive synthesis of the subject, but rather a vehicle to present new data, new ideas and alternative views. Some of the papers present regional summaries, others attempt to relate local features to regional questions, while others describe modern rift basins as possible analogs of early Mesozoic basins. Geologic data from the Atlantic passive margins record that continental rifting of central Pangaea occurred during the Late Triassic - Early Jurassic (Liassic), and that sea-floor spreading probably began no later than the Middle Jurassic. The primary subject of this book focusses on the Triassic - Jurassic rifting events that led to the breakup of Pangaea and the opening of the central Atlantic Ocean. Whereas other treatises have focused on the origin of the passive margins, inferred primarily from geophysical data of the offshore basins, this volume primarily and uniquely focuses on land-based field studies of the onshore synrift basins. Offshore studies of synrift basins are also included in this volume, for they add substantially to our understanding of the breakup. However, the onshore data base, while complementary, is different, thus providing researchers with a different insight to the ques- tions at hand. This volume brings together 39 research papers contributed by an international team of 75 geologists from 12 countries. Each paper has been reviewed by 2 outside reviewers, and originally accepted for publication in the AAPG-sponsored Memoir: Triassic and Liassic Rif- ting. Financial exigency on the part of the AAPG during the later part of 1986, however, caused the Society to postpone indefinitely the publication of this Memoir, compelling us to seek another publisher. We greatfully acknowledge the help and support of Elsevier Science Publishers. The book is organized in 4 sections. Section 1, Pangaean Plate in Time and Space, first locates Pangaea in space and then places the Triassic basins within an historical context on the Alleghanian - Variscan Orogen. Section 2, the Offshore and Onshore Basins of the North American and African Plates, comprises about 70% of all the papers in this book; it includes papers on structural geology, petrology, paleontology, sedimentation, organic geochemistry, vulcanism and mineral resources. Sections 3, Related Mesozoic Atlantic Rift Basins, includes papers on Iberia, Western Europe, the Benue trough and Brazil. The final section of the book, Analogs, includes the rift basins of East Africa, the Red Sea, the Gulf of Elat (Aqaba), the Dead Sea, and the Rio Grande. VI Preface Although it is impossible to acknowledge the support of all the individuals who have con- tributed to the successful completion of this book, I am particularly indebted to each authors for their contribution to this book and to the cadre of reviewers who have given generously of their time and expertise. I am most grateful also to Ms. Ann Kutyla, Rutgers. Newark Geology Department, whose willing cooperation has contributed markedly to the successful completion of this book. To Mrs. Katherine Pyle, University of Tulsa, for her incisive com- ments and re-organization of several early manuscripts. And finally to my wife, Sylvia, my children, David, Michele, Ilyssa and Neil, and to friends and students for their patience and understanding, particularly on those bad days. WARREN MANSPEIZER List of Contributors CARLOS L.V. AIKEN HAROLD L. COUSMINER Center for Lithospheric Studies, U.S. Department of the Interior, University of Texas at Dallas, Minerals Management Service, Richardson, TX 75080, U.S.A. Pacific OCS Region, 1340 W. Sixth Street, ALFREDO ARCHE Los Angeles, CA 90017, U.S.A. Dept. Estratigrafia, Univ. Complutense, P. DAINELLI Madrid 28040, Spain GEOMAP, Florence, Italy JACQUES BEAUCHAMP Departement de Geologie, JELLE ZEILINGA DE BOER Universite de Picardie, Department of Earth & Environmental Sciences, 80039 Amiens, France Wesleyan University, Middletown, CT 06457, U.S.A. J. BENKHELIL Departement de Geologie, S. DERKSEN Universite de Dakar, Marathon Oil Co., Dakar, Senegal P.O. Box 269, Littleton, Colo., U.S.A. RICHARD N. BENSON Delaware Geological Survey, ROBERT G. DOYLE University of Delaware, Robert G. Doyle & Assoc, Newark, DE 19716, U.S.A. 10 E. Woodtimber Court, The Woodlands, TX 77381, U.S.A. CARL F. BURGESS Exxon Company, U.S.A. P.O. Box 61812, J.D. FAIRHEAD New Orleans, LA 70161, U.S.A. Department of Earth Sciences, The University of Leeds, C.A. BURGESS Leeds, LS2 9JT, U.K. Project PROBE, Department of Geology, F.D. FOLEY Duke University, Texaco, Inc., Durham., N.C., U.S.A. Southern Exploration Division, New Orleans, LA 70130, U.S.A. GAIL P. CLEMENT Ocean Drilling Program, MICHAEL F. FORLENZA Texas A & M, ESSO Exploration Inc., University Research Park, Houston, TX 77001, U.S.A. College Station, TX 77840, U.S.A. GERALD M. FRIEDMAN AMY E. CLIFFORD Dept. of Geology, Department of Earth & Environmental Sciences, Brooklyn College City University of New York, Wesleyan University, New York, NY 12181, U.S.A. Middletown, CT 06457, U.S.A. viii List of Contributors PAMELA J.W. GORE BARRY J. KATZ Department of Geology, Texaco Inc., Emory University, Exploration & Production Atlanta, GA 30322, U.S.A. Technology Division, 3901 Briar Park, POL GUENNOC Houston, TX 77042, U.S.A. Bureau de Recherches Geologiques et Minieres, B.P. 337, G. RANDY KELLER 29273 Brest Cedex, France Department of Geological Sciences, University of Texas at El Paso, SANTIAGO HERNANDO El Paso, TX 79968, U.S.A. Dept. Estratigrafia, Univ. Complutense, KIM D. KLITGORD Madrid, 28040 Spain U.S. Geological Survey, Woods Hole, MA 02543, U.S.A. WILLIAM T. HOLSER Department of Geology, J. LAMBIASE University of Oregon, Marathon Oil Company, Eugene, OR 97403, U.S.A. P.O. Box 269, Littleton, Colo., U.S.A. JAMES D. HOOVER Department of Geological Sciences, MARCOS C. LANA University of Texas at El Paso, Petrobras Research Center (CENPES), El Paso, TX 79968, U.S.A. Rio De Janeiro, Brazil 21910 JOHN F. HUBERT EDGARD LAVILLE Department of Geology/Geography, Departement de Geologie-Laboratoire University of Massachusetts, de Geologie de Normandie Occidentale, Amherst, MA 01003, U.S.A. Universite de Caen, Esplanade de La Paix, JOSEPH HULL 14032 Caen Cedex, France Geology Department, Rutgers University, JOSE LOPEZ 195 University Ave., Dept. Estratigrafia, Newark, NJ 07102, U.S.A. Univ. Complutense, Madrid, 28040 Spain DEBORAH R. HUTCHINSON U.S. Geological Survey, MARK LUCAS Woods Hole, MA 02543, U.S.A. Geology Department, LUBOMIR F. JANSA Rutgers University, Atlantic Geoscience Center, Newark, NJ 07102, U.S.A. Geological Survey of Canada, Box 1006, R. LUTZ Dartmouth, N.S. B24 4AZ, Canada Department of Geological Sciences, Old Dominion University, T. JORJORIAN Norfolk, VA 23508, U.S.A. Texaco Inc., Exploration & Production WARREN MANSPEIZER Technology Division, Geology Department, 3901 Briar Park, Rutgers University, Houston, TX 77042, U.S.A. Newark, NJ 07102, U.S.A. ELI KASHAI J. GREGORY Mc HONE Oil Exploration Ltd., Department of Geological Sciences, P.O. Box 50199, University of Kentucky, Tel Aviv, 61500 Israel Lexington, KY 40506-0059, U.S.A. List of Contributors IX N. MEADER GEORGES POUIT Marathon Oil Company, Bureau de Recherches Geologiques P.O. Box 269, et Minieres, Littleton, Colo., U.S.A. B.P. 6009, 45060 Orleans Cedex, France KEVIN L. MICKUS Department of Geological Sciences, JOHN H. PUFFER University of Texas at El Paso, Geology Department, El Paso, TX 79968-055, U.S.A. Rutgers University, Newark, NJ 07102, U.S.A. EDISON J. MILANI Petrobras Research Center (CENPES), Rio de Janeiro, Brazil 21910 AMPARO RAMOS Dept. Estratigrafia, ZOHAIR NAWAB Univ. Complutense, Saudi-Sudanese Red Sea Joint Commission, Madrid, 28040 Spain P.O. Box 5886, Jeddah, Saudi Arabia NICHOLAS RAST Department of Geology, PAUL E. OLSEN Bowman Hall, Lamont-Doherty Geological Observatory, The University of Kentucky, Columbia University, Lexington, KY 40506, U.S.A. Palisades, NY 10964, U.S.A. ROBERT RESSETAR MARTHA E. OSHCHUDLAK Earth Sciences & Resources Institute, Fred C. Hart Associates, Inc., University of South Carolina, P.O. Box 8248, Columbia, SC 29208, U.S.A. Cherry Hill, NJ 08003, U.S.A. WAYNE J. PEEPLES ELEANORA I. ROBBINS Department of Geological Sciences, U.S. Geological Survey, University of Texas at El Paso, Reston, VA 22092, U.S.A. El Paso, TX 79968-0555, U.S.A. COLEMAN R. ROBISON MARTA PEREZ-ARLUCEA Texaco Inc., Dept. Estratigrafia, Exploration & Production Univ. Complutense, Technology Division, Madrid, 28040 Spain 3901 Briarpark, Houston, TX 77042, U.S.A. ANTHONY R. PHILPOTTS Department of Geology & Geophysics G.R. ROBINSON, Jr. University of Connecticut U.S. Geological Survey, Storrs, CT 06268 954 National Center, Reston, VA 22092, U.S.A. J.F. PONSARD 3 Laboratoire de Geologie Dynamique, SAMUEL ROOT U.A. CNRS 132, Department of Geology, Universite d'Aix, The College of Wooster, Marseille III, France Wooster, OH 44691, U.S.A. M. POPOFF, 3 Laboratoire de Geologie Dynamique, BRUCE R. ROSENDAHL U.A. CNRS 132, Project PROBE, Universite d'Aix, Duke University, Marseille III, France Durham, N.C., U.S.A. X List of Contributors S. SANDER WILLIAM A. THOMAS Project PROBE, Department of Geology, Department of Geology, University of Alabama, Duke University, Tuscaloosa, AL 35487-1945, U.S.A. Durham, N.C., U.S.A. ROB VAN DER VOO L. SAUGY Department of Geological Sciences, 4 Elf Nigeria, University of Michigan, Lagos, Nigeria Ann Arbor, MI 48109-1063, U.S.A. MICHAEL A. SMITH R. VENKATAKRISHNAN Texaco Inc., Department of Geological Sciences, E & P Technology Division, Old Dominion University, 3901 Briarpark Norfolk, VA 23508, U.S.A. Houston, TX 77042, U.S.A. CARMINA VIRGILI JOSEPH P. SMOOT Dept. Estratigrafia, Branch of Eastern Regional Geology, Univ. Complutense, U.S. Geological Survey, Madrid, 28040 Spain Reston, VA 22092, U.S.A. JOHN A. WADE ALFONSO SOPENA Atlantic Geoscience Center, Dept. Estratigrafia, Geological Survey of Canada, Univ. Complutense, Box 1006, Madrid, 28040 Spain Dartmouth, N.S. B2Y 4A2, Canada WILLIAM E. STEINKRAUS H.J. WELSINK Chevron Overseas Petroleum, Petro-Canada Resources, 6001 Bolinger Canyon Rd., P.O. Box 2844, P.O. Box 5046, Calgary, Alta. T2P 3E3, Canada San Ramon, CA 94583-0946, U.S.A. DAVID WHITTINGTON PETER SZATMARI ATC, 1635 Pumphrey Ave. Petrobras Research Center (CENPES), Auburn, AL 36830-4303, U.S.A. Rio de Janeiro, Brazil 21910 GERALD P. WILKES A.J. TANKARD Virginia Division of Mineral Resources, Petro-Canada Resources, Charlottesville, VA 22903, U.S.A. P.O. Box 2844, Calgary, Alta. T2P 2E3, Canada DANIEL G. ZIEGLER Southeastern Exploration & Production Company, G.K. TAYLOR Dallas, TX 75201, U.S.A. Groundwater Protection Division, SC Department of Health & Environmental P.A. ZIEGLER Control, Shell Internationale Petroleum 2600 Bull Street, Maatschappij B.V., Columbia, SC 29201, U.S.A. P.O. Box 162, 2501 AN The Hague, The Netherlands DANIEL A. TEXTORIS University of North Carolina, Chapel Hill, NC 27514, U.S.A. Chapter 1 Variscan - Alleghanian orogen N. RAST ABSTRACT The Variscan - Alleghanian orogen stretches from the southeastern United States to eastern Europe and fragments of it are also detected in eastern and northeastern Africa. The orogen has originally been produced by the collision between Gondwana, Laurentian and Baltic cratons, as well as the intervening microcontinents. As a result of postorogenic erosion, superposed sedimentation and Mesozic and Tertiary rifting and compressive episodes the orogen is divided into separated segments and massifs. The north-northwestern edge of the orogen, marked by the northern Variscan thrust and deformation front, indicates tectonic transport to the north-northwest, while the south-southeastern edge of the orogen similarly delineated by the southern Variscan front shows tectonic transport to the south-southeast. This polarity is the strongest evidence for the continental collision causing Variscan- Alleghanian orogeny. Within the fronts the orogen can be divided into the internides and the northern and southern externides. The internides are characterized by variable, but commonly high-grade metamorphism and granitic intrusions. The nor- thern externides are weakly metamorphosed, generally devoid of granites, and strongly affected by overthrusting. The southern externides have had similar features but are heavily overprinted by the Alpine structures. Several lines can be suggested as collisional sutures. The orogen forms a foundation to the postorogenic Permo-Triassic deposits. Introduction Following the original work of Suess (1885 - 1909) in Europe it has become customary to delineate orogenic belts on a world-wide scale. Although lately there has been a waning in enthusiasm for this usage, the tradition in many cases still persists. In this paper, the Variscan - Alleghanian orogen is restricted to western and central Europe and parts of North Africa, as well as eastern North America. In Europe eastwards, I place the limit to the belt against a fault system known as the Tornquist line (Fig. 1-1), while in North America I restrict it to the Appalachian system and consider the Ouachitas to be broadly synchronous but a separate system. The east-southeastern part of the orogen then includes the Mauritanides of West Africa as well as overprinted Variscan structures within the Alpine orogenic belt. While manifestations of Variscan (Hercynian) orogenic events have been claimed from the Caucasus, Iran, Soviet Turkestan, etc., I think it is sensible to restrict the definition to the irregular crescentic region margined by the Laurentian and Baltic cratons (Laurasia) on one side and the African craton on the other. In this region, numerous in- vestigations indicate a distinct polarity of folds and thrust faults and therefore of tectonic transport. This is shown in Figure 1-1, which has been constructed principally on the basis of information provided by Hatcher and Odom (1980), Geiser and Engelder (1983) and Rast et al. (1984) in North America, by Shackleton et al. (1982) in Britain, by Krebs (1977), Matte (1983) and Vai (1979) in Europe, by Michard (1978), Dillon and Sougy (1974) and Conrad and Lemosquet (1984) in North Africa, and by Bourrouilh and Gorsline (1979) in the western Mediterranean area. The mirror symmetry of vergence of Variscan structures indicates that

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Extensive field studies on the African and North American plates during this past decade have yielded a wealth of new data and ideas about rift basins and the origin of passive margins. New surface and subsurface basins have been identified; fossils abound in strata that only recently were considere
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Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.