Total Petroleum Systems of the Paleozoic and Jurassic, Greater Ghawar Uplift and Adjoining Provinces of Central Saudi Arabia and Northern Arabian-Persian Gulf

Total Page:16

File Type:pdf, Size:1020Kb

Total Petroleum Systems of the Paleozoic and Jurassic, Greater Ghawar Uplift and Adjoining Provinces of Central Saudi Arabia and Northern Arabian-Persian Gulf Total Petroleum Systems of the Paleozoic and Jurassic, Greater Ghawar Uplift and Adjoining Provinces of Central Saudi Arabia and Northern Arabian-Persian Gulf U.S. Geological Survey Bulletin 2202-H U.S. Department of the Interior U.S. Geological Survey Total Petroleum Systems of the Paleozoic and Jurassic, Greater Ghawar Uplift and Adjoining Provinces of Central Saudi Arabia and Northern Arabian-Persian Gulf By Richard M. Pollastro U.S. Geological Survey Bulletin 2202-H U.S. Department of the Interior U.S. Geological Survey iii U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director Version 1.0, 2003 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ This publication is only available online at: http://pubs.usgs.gov/bul/b2202-h/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. iii U.S. Department of the Interior Contents Gale A. Norton, Secretary U.S. Geological Survey Foreword ........................................................................................................................................................ 1 Charles G. Groat, Director Abstract.......................................................................................................................................................... 3 Introduction ................................................................................................................................................... 3 Acknowledgments........................................................................................................................................ 6 U.S. Geological Survey Geologic Provinces of Central Saudi Arabia and Gulf Area........................ 6 Greater Petroleum Systems of the Eastern Arabian Peninsula............................................................ 9 Tectonic Evolution and Structural Setting................................................................................................ 9 Version 1.0, 2003 Stratigraphy of Central Saudi Arabia and Greater Ghawar Region ................................................... 18 Pre-Khuff Section................................................................................................................. 18 Late Permian Through Jurassic......................................................................................... 20 Central Arabia Qusaiba-Paleozoic Total Petroleum System ............................................................... 24 General Description............................................................................................................. 24 For more information about the USGS and its products: Petroleum Geochemistry .................................................................................................... 24 Telephone: 1-888-ASK-USGS Source Rocks............................................................................................................... 24 World Wide Web: http://www.usgs.gov/ Organic Geochemistry................................................................................................ 29 Maturation, Generation, and Expulsion................................................................... 29 This publication is only available online at: Reservoirs.............................................................................................................................. 39 http://pubs.usgs.gov/bul/b2202-h/ Seal Rocks............................................................................................................................. 42 Traps and Trap Styles .......................................................................................................... 42 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply Arabian Sub-Basin Tuwaiq/Hanifa-Arab Total Petroleum System..................................................... 44 endorsement by the U.S. Government. General Description............................................................................................................. 44 Petroleum Geochemistry .................................................................................................... 44 Source Rocks............................................................................................................... 44 Organic Geochemistry................................................................................................ 49 Maturation, Generation, and Expulsion................................................................... 49 Reservoirs.............................................................................................................................. 52 Seal Rocks............................................................................................................................. 56 Traps and Trap Styles .......................................................................................................... 56 Assessment Unit Description, Geologic Models, and Assessment Results..................................... 57 Central Arabia Qusaiba-Paleozoic TPS............................................................................ 57 Central Arch Horst-Block Anticlinal Oil and Gas AU (20210101) ......................... 57 North Gulf Salt Basin Structural Gas AU (20210102) ............................................. 65 Arabian Sub-Basin Tuwaiq/Hanifa-Arab TPS ................................................................. 65 Horst-Block Anticlinal Oil AU (20210201)................................................................. 65 Salt-Involved Structural Oil AU (20210202) ............................................................. 68 Summary ...................................................................................................................................................... 72 Selected References.................................................................................................................................. 75 Appendix 1. Seventh Approximation Input Form for Central Arch Horst-Block Anticlinal Oil and Gas Assessment Unit (20210101), Central Arabia Qusaiba-Paleozoic Total Petroleum System................................................................................................................ 81 Appendix 2. Seventh Approximation Input Form for North Gulf Salt Basin Structural Gas Assessment Unit (20210102), Central Arabia Qusaiba-Paleozoic Total Petroleum System ......................................................................................................................... 86 iv v Appendix 3. Seventh Approximation Input Form for Horst-Block Anticlinal Oil Assessment Unit (20210201), Arabian Sub-Basin Tuwaiq/Hanifa-Arab Total Petroleum System................................................................................................................ 91 Appendix 4. Seventh Approximation Input Form for Salt-Involved Structural Oil Assessment Unit (20210202), Arabian Sub-Basin Tuwaiq/Hanifa-Arab Total Petroleum System........... 96 Figures 1. Diagram showing stratigraphic section, major tectonic events, and stratigraphic units of petroleum systems of the eastern Arabian Peninsula............................................ 4 2–7. Maps showing: 2. USGS geologic provinces of central Saudi Arabia and northern Arabian-Persian Gulf, and details of oil and gas fields and reservoirs........................................................ 5 3. Arabian Plate showing general tectonic and structural features, salt basins, and oil and gas fields........................................................................................................................... 7 4. Jurassic intraplatform sub-basins of Arabian-Persian Gulf region................................ 8 5. Paleozoic and Jurassic total petroleum systems of Gotnia sub-basin........................ 10 6. USGS geologic provinces, oil and gas field centerpoints, and total petroleum systems of central Saudi Arabia and northern Arabian-Persian Gulf.......................... 11 7. Cretaceous, Jurassic, and Paleozoic total petroleum systems and oil and gas field centerpoints of Rub’al Khali Province (2019).................................................................... 12 8. Sketch block diagrams showing evolution of Arabian Plate tectonics............................ 14 9. Geologic cross section across Saudi Arabia and Qatar..................................................... 15 10. Geologic subcrop map of Hercynian or “Pre-Unayzah” unconformity............................ 16 11. Structural cross section of central Ghawar field................................................................. 17 12. Chart showing growth history of major tectonic events and relative intensities........... 19 13. Diagram showing stratigraphic column and tectonostratigraphic events of the Paleozoic section in Greater Ghawar area........................................................................... 21 14. General stratigraphic section of the Upper Jurassic Arab Formation ............................. 23 15. Map showing Central Arabia Qusaiba-Paleozoic Total Petroleum System and assessment units ............................................................................................................... 25 16. Paleoenvironmental map of the Early Silurian showing approximate
Recommended publications
  • Fish and Fishing
    CHAPTER TWELVE Fish and Fishing D.T. Potts 1 Introduction The benefi ts of fi sh in the human diet have long been recognized. With an average protein content of 18 – 22 percent and other important elements (essential amino acids, calcium, fl ourine, iodine, iron, phosphorus; Vitamins A, B, and D), fi sh have been an important component of the low - protein, high - carbohydrate diets that have been common in the Near East throughout the pre - Modern era (Englund 1990 : 7 n33; see in general Van Neer 1994 ). Nowadays, the benefi ts of Omega 3 fatty acids in fi sh oil are promoted for their ability to help the body combat everything from Alzheimer ’ s disease to cancer, ulcers, and many more affl ictions. Nevertheless, considering the fact that the region dealt with in this volume contains long stretches of shoreline on at least seven seas (Aegean, Medi- terranean, Black, Red, Caspian and Arabian Seas, and the Persian Gulf), as well as a number of major rivers (Tigris, Euphrates, Karun, Orontes, Khabur, Balikh, Jordan, Greater Zab) and lakes (e.g., Lake Kinneret, Lake Van, Lake Parishan, Hamun - e Helmand), not to mention thousands of manmade irrigation canals, neither freshwater nor saltwater fi sh in Near Eastern antiquity have received the attention that they deserve. The purpose of this chapter is to provide a broad overview of a number of issues associated with fi sh. Topics discussed below include fi sh remains in archaeological contexts; evidence of fi shing sites; fi shing techniques and equipment; written sources on the organization of fi shing; fi sh preparation for consumption and the dietary contribution of fi sh in antiquity; A Companion to the Archaeology of the Ancient Near East, First Edition.
    [Show full text]
  • Saudi Arabia.Pdf
    A saudi man with his horse Performance of Al Ardha, the Saudi national dance in Riyadh Flickr / Charles Roffey Flickr / Abraham Puthoor SAUDI ARABIA Dec. 2019 Table of Contents Chapter 1 | Geography . 6 Introduction . 6 Geographical Divisions . 7 Asir, the Southern Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �7 Rub al-Khali and the Southern Region � � � � � � � � � � � � � � � � � � � � � � � � � �8 Hejaz, the Western Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �8 Nejd, the Central Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �9 The Eastern Region � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �9 Topographical Divisions . .. 9 Deserts and Mountains � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �9 Climate . .. 10 Bodies of Water . 11 Red Sea � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 11 Persian Gulf � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 11 Wadis � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � 11 Major Cities . 12 Riyadh � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �12 Jeddah � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �13 Mecca � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � �
    [Show full text]
  • Gondwana Large Igneous Provinces (Lips): Distribution, Diversity and Significance
    Downloaded from http://sp.lyellcollection.org/ by guest on September 25, 2021 Gondwana Large Igneous Provinces (LIPs): distribution, diversity and significance SARAJIT SENSARMA1*, BRYAN C. STOREY2 & VIVEK P. MALVIYA3 1Centre of Advanced Study in Geology, University of Lucknow, Lucknow, Uttar Pradesh 226007, India 2Gateway Antarctica, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand 324E Mayur Residency Extension, Faridi Nagar, Lucknow, Uttar Pradesh 226016, India *Correspondence: [email protected] Abstract: Gondwana, comprising >64% of the present-day continental mass, is home to 33% of Large Igneous Provinces (LIPs) and is key to unravelling the lithosphere–atmosphere system and related tectonics that mediated global climate shifts and sediment production conducive for life on Earth. Increased recognition of bimodal LIPs in Gondwana with significant, sometimes subequal, proportions of synchronous silicic volcanic rocks, mostly rhyolites to high silica rhyolites (±associ- ated granitoids) to mafic volcanic rocks is a major frontier, not considered in mantle plume or plate process hypotheses. On a δ18O v. initial 87Sr/86Sr plot for silicic rocks in Gondwana LIPs there is a remarkable spread between continental crust and mantle values, signifying variable contributions of crust and mantle in their origins. Caldera-forming silicic LIP events were as large as their mafic counterparts, and erupted for a longer duration (>20 myr). Several Gondwana LIPs erupted near the active continental margins, in addition to within-continents; rifting, however, continued even after LIP emplacements in several cases or was aborted and did not open into ocean by coeval com- pression. Gondwana LIPs had devastating consequences in global climate shifts and are major global sediment sources influencing upper continental crust compositions.
    [Show full text]
  • Y-Chromosome & Mitochondrial DNA Variation
    The Genetic Structure of the Kuwaiti and Failaka Island Populations: Y-chromosome & Mitochondrial DNA Variation By Jasem Bader Theyab M.A., University of Kansas, 2010 Copyright 2013 Submitted to the graduate degree program in Anthropology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Doctor of Philosophy. ________________________________ Chairperson, Dr. Michael H. Crawford ________________________________ Dr. Majid Hannoum ________________________________ Dr. Deborah Smith ________________________________ Dr. Bartholomew C. Dean ________________________________ Dr. John Kelly Date Defended: May 28, 2013 The Dissertation Committee for Jasem Bader Theyab certifies that this is the approved version of the following dissertation: The Genetic Structure of the Kuwaiti and Failaka Island Populations: Y-chromosome & Mitochondrial DNA Variation ________________________________ Chairperson, Dr. Michael H. Crawford Date approved: May 31, 2013 ii Abstract Recent studies applying multidisciplinary approaches suggest that the Anatomically Modern Homo sapiens (AMHS) passed through the Arabian Peninsula in their major diaspora out of Africa. The Arabian Peninsula is connected to three continents: Africa, Asia, and Europe. In addition to the major diaspora, the Arabian Peninsula has witnessed numerous migrations among the three continents. The populations of the Arabian Peninsula have been investigated to better understand their evolutionary history. This dissertation investigated the paternal genetic structure of the Kuwaiti and Failaka Island populations using 15 loci Y-STR data. In addition, the maternal genetic structure of Failaka Island has been investigated using mtDNA HVS-I sequence data. This is the first genetic study to characterize Failaka Island population. The result showed that the Kuwaiti population has a high frequency of Y- haplogroup J1 (37%) similar to other Arabian populations.
    [Show full text]
  • Arabian Peninsula from Wikipedia, the Free Encyclopedia Jump to Navigationjump to Search "Arabia" and "Arabian" Redirect Here
    Arabian Peninsula From Wikipedia, the free encyclopedia Jump to navigationJump to search "Arabia" and "Arabian" redirect here. For other uses, see Arabia (disambiguation) and Arabian (disambiguation). Arabian Peninsula Area 3.2 million km2 (1.25 million mi²) Population 77,983,936 Demonym Arabian Countries Saudi Arabia Yemen Oman United Arab Emirates Kuwait Qatar Bahrain -shibhu l-jazīrati l ِش ْبهُ ا ْل َج ِزي َرةِ ا ْلعَ َربِيَّة :The Arabian Peninsula, or simply Arabia[1] (/əˈreɪbiə/; Arabic jazīratu l-ʿarab, 'Island of the Arabs'),[2] is َج ِزي َرةُ ا ْلعَ َرب ʿarabiyyah, 'Arabian peninsula' or a peninsula of Western Asia situated northeast of Africa on the Arabian plate. From a geographical perspective, it is considered a subcontinent of Asia.[3] It is the largest peninsula in the world, at 3,237,500 km2 (1,250,000 sq mi).[4][5][6][7][8] The peninsula consists of the countries Yemen, Oman, Qatar, Bahrain, Kuwait, Saudi Arabia and the United Arab Emirates.[9] The peninsula formed as a result of the rifting of the Red Sea between 56 and 23 million years ago, and is bordered by the Red Sea to the west and southwest, the Persian Gulf to the northeast, the Levant to the north and the Indian Ocean to the southeast. The peninsula plays a critical geopolitical role in the Arab world due to its vast reserves of oil and natural gas. The most populous cities on the Arabian Peninsula are Riyadh, Dubai, Jeddah, Abu Dhabi, Doha, Kuwait City, Sanaʽa, and Mecca. Before the modern era, it was divided into four distinct regions: Red Sea Coast (Tihamah), Central Plateau (Al-Yamama), Indian Ocean Coast (Hadhramaut) and Persian Gulf Coast (Al-Bahrain).
    [Show full text]
  • General: Anonymous. Periplus Maris Erythraei (Or 'Voyage Around The
    General: Anonymous. Periplus Maris Erythraei (or ‘Voyage around the Erythraean Sea’). L. Casson. The Periplus Maris Erythraei: Text with Introduction, Translation, and Commentary. Princeton (1989). Cosmas Indicopleustes. Christian Topography. Boivin, N., Blench, R., & Fuller, D. (2009). Archaeological, linguistic and historical sources on ancient seafaring: A multidisciplinary approach to the study of early maritime contact and exchange in the Arabian Peninsula. In M. Petraglia & J. Rose (Eds.), The evolution of human populations in Arabia (pp. 251–278). New York: Springer. S. Faller. "The World According to Cosmas Indicopleustes—Concepts and Illustrations of an Alexandrian Merchant and Monk." M. P. Fitzpatrick. "Provincializing Rome: The Indian Ocean Trade Network and Roman Imperialism." Journal of World History 22 (2011): 27–54. S. Sidebotham. "The Red Sea and Indian Ocean in the Age of the Great Empires." In A Companion to the Archaeology of the Ancient Near East, ed. D. Potts, 1041-1059. (2012). Week One: Roman Egypt and Late Antique Egypt K. Damgaard, "A Palestinian Red Sea Port on the Egyptian Road to Arabia: Early Islamic Aqaba and its Many Hinterlands." In L. Blue – J. Cooper – R. Thomas – J. Whitewright (eds.), Connected Hinterlands: Proceedings of the Red Sea Project IV Held at the University of Southampton, September 2008, 85-98. Oxford (2009). S. Sidebotham. "Trade in Roman Berenike." In Berenike and the Ancient Maritime Spice Route. Berkeley and Los Angeles (2011), 221–258. S. Sidebotham. "Other Emporia." In Berenike and the Ancient Maritime Spice Route, 175-194. Berkeley and Los Angeles (2011). J. Whitewright. "The Ships and Shipping of Indo-Roman Trade: A View from Egyptian Red Sea Ports." Herom 6 (2017): 137-172.
    [Show full text]
  • Geologic History of Water on Mars
    GEOLOGIC HISTORY OF WATER ON MARS: REGIONAL EVOLUTION OF AQUEOUS AND GLACIAL PROCESSES IN THE SOUTHERN HIGHLANDS, THROUGH TIME Dissertation zur Erlangung des akademischen Grades eines Doktors der Naturwissenschaften (Dr. rer. nat) vorgelegt als kumulative Arbeit am Fachbereich Geowissenschaften der Freien Universität Berlin von SOLMAZ ADELI Berlin, 2016 Erstgutachter: Prof. Dr. Ralf Jaumann Freie Universität Berlin Institut für Geologische Wissenschaften Arbeitsbereich Planetologie sowie Deutsches Zentrum für Luft- und Raumfahrt Institut für Planetenforschung, Abteilung Planetengeologie Zweitgutachter: Prof. Dr. Michael Schneider Freie Universität Berlin Institut für Geologische Wissenschaften Arbeitsbereich Hydrogeologie Tag der Disputation: 22 July 2016 i To my mother and my grandmother, the two strong women who inspired me the most, to follow my dreams, and to never give up. تقديم به مادر و مادر بزرگم به دو زن قوى كه الهام دهنده ى من بودند تا آرزو هايم را دنبال كنم و هرگز تسليم نشوم ii iii EIDESSTATTLICHE ERKLAERUNG Hiermit versichere ich, die vorliegende Arbeit selbstständig angefertigt und keine anderen als die angeführten Quellen und Hilfsmittel benutzt zu haben. Solmaz Adeli Berlin, 2016 iv v Acknowledgement First of all, I would like to thank my supervisor Prof. Dr. Ralf Jaumann for giving me the opportunity of working at the Deutsches Zentrum für Luft- und Raumfahrt (DLR). I wish to thank him particularly for standing behind me in all the ups and downs. Herr Jaumann, I am so deeply grateful for your support and your trust. Danke schön! This work would have not been achieved without the support of Ernst Hauber, my second supervisor. I have also been most fortunate to be able to work with him, and I have greatly appreciated the countless hours of discussions, all his advice regarding scientific issues, his feedbacks on my manuscripts, and everything.
    [Show full text]
  • Math + X Symposium on Seismology and Inverse Problems Rice University · January 24–26, 2018
    Math + X Symposium on Seismology and Inverse Problems Rice University · January 24–26, 2018 funded by Math + X Symposium on Data Science and Inverse Problems in Geophysics Rice University · January 24–26, 2018 BioScience Research Collaborative (BRC) Building, Room 280 Wednesday, January 24th 8:15am Maarten de Hoop Welcome Reginald DesRoches Opening Remarks 8:30am Nathan Ku Data-driven discovery of governing physical laws and their parametric dependencies in engineering, physics and biology 9:20am Michel Campillo From ”ambient noise” to seismic imaging and monitoring 10:10am BREAK 10:35am András Vasy Global analysis via microlocal tools: Fredholm problems in non-elliptic seings 11:25am Andrew Stuart Large graph limits of learning algorithms 12:15pm LUNCH 1:15pm Mai Lassas Manifold learning and an inverse problem for a wave equation 2:05pm Frederik Simons On the inversion of noisy, incomplete, scaered, and vector-valued satellite-data for planetary magnetic-field models 2:55pm BREAK 3:20pm Elchanan Mossel Hierarchal generative models and deep learning 4:10pm Andrea Bertozzi Geometric graph-based methods for high dimensional data 6:00pm RECEPTION, RICE FACULTY CLUB Cohen House, 6100 Main St. Cocktails and Appetizers, Event Parking ** Registrants are provided a daily boxed lunch ** For venue locations and parking information please see: hps://earthscience.rice.edu/mathx2018/ Thursday, January 25th 8:30am Gregory Beroza FAST: a data-mining approach for earthquake detection 9:20am Ankur Moitra Robustness meets algorithms 10:10am BREAK 10:35am
    [Show full text]
  • By Lee A. Breakiron ONE-SHOT WONDERS
    REHeapa Autumnal Equinox 2015 By Lee A. Breakiron ONE-SHOT WONDERS By definition, fanzines are nonprofessional publications produced by fans of a particular cultural phenomenon, such as a literary or musical genre, for the pleasure of others who share their interests. Readers themselves often contribute to fanzines by submitting their own articles, reviews, letters of comment, and fan fiction. Though the term fanzine only dates from 1940 when it was popularized within science fiction and comic book fandom, the first fanzines actually date back to at least the nineteenth century when, as a uniquely American development, literary groups formed amateur press associations or APAs in order to publish collections of poetry, fiction, and commentary. Few, if any, writers have had as many fanzines, chapbooks, and other ephemera dedicated to them as has Robert E. Howard. Howard himself self-published his own typed “zine,” The Golden Caliph of four loose pages in about August, 1923 [1], as well as three issues of one entitled The Right Hook in 1925 (discussed later). Howard collaborated with his friends Tevis Clyde “Clyde” Smith, Jr., and Truett Vinson in their own zines, The All-Around Magazine and The Toreador respectively, in 1923 and 1925. (A copy of The All-Around Magazine sold for $911 in 2005.) Howard also participated in an amateur essay, commentary, and poetry journal called The Junto that ran from 1928 to 1930, contributing 10 stories and 13 poems to 10 of the issues that survive. Only one copy of this monthly “travelogue” was circulated among all the members of the group.
    [Show full text]
  • Petrofacies and Paleotectonic Evolution of Permo-Carboniferous Gondwanan Sequences of the Bengal Basin, Bangladesh
    Petrofacies and Paleotectonic Evolution of Permo-Carboniferous Gondwanan Sequences of the Bengal Basin, Bangladesh by Md. Iftekhar Alam A thesis submitted to the Graduate Faculty of Auburn University in partial fulfillment of the requirements for the Degree of Master of Science Auburn, Alabama December 12, 2011 Keywords: Gondwanaland, Petrofacies, Paleotectonic, Permo-Carboniferous, Bangladesh Copyright 2011 by Md. Iftekhar Alam Approved by Ashraf Uddin, Chair, Professor of Geology Charles E. Savrda, Professor of Geology David T. King, Jr., Professor of Geology Willis E. Hames, Professor of Geology Abstract The Indian subcontinent, along with Australia and Antarctica, constituted Eastern Gondwananland. Permo-Carboniferous Gondwanan sequences have been reported from several isolated basins of the Peninsular India. These siliciclastic sequences were drilled in intra-cratonic basins in northwest Bengal Basin. This ~1-km-thick sequence consists primarily of massive and trough cross-bedded sandstones and laminated mudstones, with localized conglomerate and coal layers. Sandstone petrography, heavy mineral assemblage studies, heavy mineral geochemistry, and detrital geochronology were used in this study to decipher provenance history of Gondwanan sediments at two localities (Khalashpir and Barapukuria) from the Bengal Basin of Bangladesh. Petrographic studies suggest that these sequences are mostly immature and poorly sorted arkosic sandstones (Khalashpir-Qt58F30L12, Barapukuria-Qt52F31L17), with some compositions ranging from quartzarenite to litharenite. Although monocrystalline quartz is dominant, considerable polycrystalline quartz fragments have also been found. K-feldspars dominate over plagioclase feldspars. Among lithic fragments, sedimentary types are abundant. Significant amounts of chert are observed. Heavy minerals are volumetrically rare and of low diversity in sediments of northwest Bangladesh. However, samples from Khalashpir have higher heavy mineral concentrations than ii those from Barapukuria.
    [Show full text]
  • Provenance of Permian-Triassic Gondwana Sequence Units
    GR-01538; No of Pages 12 Gondwana Research xxx (2015) xxx–xxx Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Provenance of Permian–Triassic Gondwana Sequence units accreted to the Banda Arc in the Timor region: Constraints from zircon U–Pb and Hf isotopes Christopher J. Spencer a,b,⁎, Ron A. Harris a, Jonathan R. Major a,c a Department of Geological Sciences, Brigham Young University, Provo, UT 84602, USA b Department of Applied Geology, Curtin University, Perth, WA 6845, Australia c Bureau of Economic Geology, University of Texas at Austin, Austin, TX 78713, USA article info abstract Article history: Analysis of zircons from Australian affinity Permian–Triassic units of the Timor region yield age distributions with Received 17 June 2015 large age peaks at 230–400 Ma and 1750–1900 Ma, which are similar to zircon age spectra found in rocks from NE Received in revised form 30 September 2015 Australia and crustal fragments now found in Tibet and SE Asia. It is likely that these terranes, which are now Accepted 14 October 2015 widely separated, were once part of the northern edge of Gondwana near what is now the northern margin of Available online xxxx Australia. The Cimmerian Block rifted from Gondwana in the Early Permian during the initial formation of the Handling Editor: A.R.A. Aitken Neo-Tethys Ocean. The zircon age spectra of the Gondwana Sequence of NE Australia and in the Timor region are most similar to the terranes of northern Tibet and Malaysia, further substantiating a similar tectonic affinity.
    [Show full text]
  • Muttoni+Kent-2019 RIPS Copy
    Rivista Italiana di Paleontologia e Stratigrafa (Research in Paleontology and Stratigraphy) vol. 125(1): 249-269. March 2019 ADRIA AS PROMONTORY OF AFRICA AND ITS CONCEPTUAL ROLE IN THE TETHYS TWIST AND PANGEA B TO PANGEA A TRANSFORMATION IN THE PERMIAN GIOVANNI MUTTONI1* & DENNIS V. KENT2 1 *Corresponding author. Dipartimento di Scienze della Terra 'Ardito Desio', Università degli Studi di Milano, via Mangiagalli 34, I-20133 Milan, Italy. 2Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08854, USA, and Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.. To cite this article: Muttoni G. & Kent D.V. (2019) - Adria as promontory of Africa and its conceptual role in the Tethys Twist and Pangea B to Pangea A Transformation in the Permian. Riv. It. Paleontol. Strat., 125(1): 249-269. Keywords: Paleomagnetism; Adria; Pangea B; Pangea A. Abstract. It has been almost 60 years since the frst results from the Early Permian Bolzano Quartz Porphyries from the Trento Plateau of northern Italy (Southern Alps) showed paleomagnetic inclinations steeper than inclina- tions from broadly coeval units from central Europe. This experimental discrepancy, confrmed ever since at varying levels of magnitude and certitude, implied that northern Italy had paleolatitudes too northerly relative to Europe to be considered part of the European continent. On the other hand, it became progressively more apparent that paleo- magnetic data from northern Italy were more compatible with data from Africa than with data from Europe, and this observation revived and complemented Argand’s original concept of Adria as a promontory of Africa. But if Adria was part of Africa, then the paleolatitude anomaly of Adria relative to Europe translated into a huge crustal misft of Gondwana relative to Laurasia when these landmasses were forced into a classic Wegenerian Pangea as typifed by the Bullard ft of the circum-Atlantic continents.
    [Show full text]