Geologic Overview and Petroleum Systems of the Greater Ghawar
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Exclusion and Citizenship in the Arab Gulf States
University of Pennsylvania ScholarlyCommons CUREJ - College Undergraduate Research Electronic Journal College of Arts and Sciences 5-15-2017 Crystallizing a Discourse of "Khalijiness": Exclusion and Citizenship in the Arab Gulf States Khaled A. Abdulkarim University of Pennsylvania, [email protected] Follow this and additional works at: https://repository.upenn.edu/curej Part of the Near Eastern Languages and Societies Commons Recommended Citation Abdulkarim, Khaled A., "Crystallizing a Discourse of "Khalijiness": Exclusion and Citizenship in the Arab Gulf States" 15 May 2017. CUREJ: College Undergraduate Research Electronic Journal, University of Pennsylvania, https://repository.upenn.edu/curej/211. A senior thesis submitted to the Huntsman Program in Business and International Studies, the University of Pennsylvania, in partial fulfillment of the program degree requirements. This paper is posted at ScholarlyCommons. https://repository.upenn.edu/curej/211 For more information, please contact [email protected]. Crystallizing a Discourse of "Khalijiness": Exclusion and Citizenship in the Arab Gulf States Abstract For many of the Arab Gulf countries, non-national populations constitute the majority of the population, with the discrepancy between the size of the national and non-national populations continuing to grow. It is in this context that the role played by these non-national populations becomes critically important. In my paper, I argue that exclusion of non-national populations from state-sponsored national identities, as manifest through citizenship rights, plays a pivotal role in fostering imagined national identities and communities among the local Arab Gulf citizens. The study considers two cases in particular: the bidoon (stateless) of Kuwait and middle-class Indian migrants in Dubai. -
Op-Ed Contributor - ‘Peak Oil’ Is a Wa…
9/4/2009 Op-Ed Contributor - ‘Peak Oil’ Is a Wa… August 25, 2009 OP-ED CONT RIBUT OR ‘Peak Oil’ Is a Waste of Energy By MICHAEL LYNCH Amherst, Mass. REMEMBER “peak oil”? It’s the theory that geological scarcity will at some point make it impossible for global petroleum production to avoid falling, heralding the end of the oil age and, potentially, economic catastrophe. Well, just when we thought that the collapse in oil prices since last summer had put an end to such talk, along comes Fatih Birol, the top economist at the International Energy Agency, to insist that we’ll reach the peak moment in 10 years, a decade sooner than most previous predictions (although a few ardent pessimists believe the moment of no return has already come and gone). Like many Malthusian beliefs, peak oil theory has been promoted by a motivated group of scientists and laymen who base their conclusions on poor analyses of data and misinterpretations of technical material. But because the news media and prominent figures like James Schlesinger, a former secretary of energy, and the oilman T. Boone Pickens have taken peak oil seriously, the public is understandably alarmed. A careful examination of the facts shows that most arguments about peak oil are based on anecdotal information, vague references and ignorance of how the oil industry goes about finding fields and extracting petroleum. And this has been demonstrated over and over again: the founder of the Association for the Study of Peak Oil first claimed in 1989 that the peak had already been reached, and Mr. -
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. -
326-97 Lab Final S.D
Geol 326-97 Name: KEY 5/6/97 Class Ave = 101 / 150 Geol 326-97 Lab Final s.d. = 24 This lab final exam is worth 150 points of your total grade. Each lettered question is worth 15 points. Read through it all first to find out what you need to do. List all of your answers on these pages and attach any constructions, tracing paper overlays, etc. Put your name on all pages. 1. One way to analyze brittle faults is to calculate and plot the infinitesimal shortening and extension directions on a lower hemisphere, stereographic projection. These principal axes lie in the “movement plane”, which contains the pole to the fault plane and the slickensides, and are at 45° to the pole. The following questions apply to a single fault described in part (a), below: (a) A fault has a strike and dip of 250, 57 N and the slickensides have a rake of 63°, measured from the given strike azimuth. Plot the orientations of the fault plane and the slickensides on an equal area projection. (b) Bedding in the vicinity of the fault is oriented 37, 42 E. Assuming that the fault formed when the bedding was horizontal, determine and plot the original geometry of the fault and the slickensides. (c) Determine the original (pre-rotation)orientation of the infinitesimal shortening and extension axes for fault. 2. All of the following questions apply to the map shown on the next page. In all of the rocks with cleavage, you may assume that both cleavage and bedding strike 024°. -
River-Gulf System—The Major Location of Marine Source Rock Formation
Pet.Sci.(2012)9:281-289 281 DOI 10.1007/s12182-012-0210-0 River-gulf system—the major location of marine source rock formation Deng Yunhua CNOOC Research Institute, Beijing 100027, China © China University of Petroleum (Beijing) and Springer-Verlag Berlin Heidelberg 2012 Abstract: Petroleum was generated from sedimentary rocks. The world’s oldest oil source rock so far was found in Proterozoic rocks. Since then, 73% to 81% of the earth’s surface has been covered with sedimentary rocks. However, only quite a limited area is rich in oil and gas. It is found that source rocks have controlled oil and gas distribution, and they are mainly formed in two systems: (1) river-lake systems and (2) river-gulf systems. Phytoplankton is an important source of kerogen, the blooming of which is strongly dependent on nutrients. Rivers are the major nutrient provider for basins. Rivers around lakes and an undercompensation (where the sedimentation rate is less than the rate of basin subsidence) environment provide favorable conditions for phytoplankton blooming in lakes. Gulfs are usually located at the estuary of big rivers, characterized by restricted current circulation and exchange with the open sea, which benefit maintaining the nutrient density, phytoplankton levels and organic matter preservation. The river-gulf system is the most favorable place for marine source rock development. Most of the world famous marine petroleum-rich provinces are developed from river-gulf systems in geological history, such as the Persian Gulf Basin, Siberian Basin, Caspian Basin, North Sea, Sirte Basin, Nigerian Basin, Kwanza Basin, Gulf of Mexico, Maracaibo Basin and the Eastern Venezuelan Basin. -
Tectonics of the Musandam Peninsula and Northern Oman Mountains: from Ophiolite Obduction to Continental Collision
GeoArabia, 2014, v. 19, no. 2, p. 135-174 Gulf PetroLink, Bahrain Tectonics of the Musandam Peninsula and northern Oman Mountains: From ophiolite obduction to continental collision Michael P. Searle, Alan G. Cherry, Mohammed Y. Ali and David J.W. Cooper ABSTRACT The tectonics of the Musandam Peninsula in northern Oman shows a transition between the Late Cretaceous ophiolite emplacement related tectonics recorded along the Oman Mountains and Dibba Zone to the SE and the Late Cenozoic continent-continent collision tectonics along the Zagros Mountains in Iran to the northwest. Three stages in the continental collision process have been recognized. Stage one involves the emplacement of the Semail Ophiolite from NE to SW onto the Mid-Permian–Mesozoic passive continental margin of Arabia. The Semail Ophiolite shows a lower ocean ridge axis suite of gabbros, tonalites, trondhjemites and lavas (Geotimes V1 unit) dated by U-Pb zircon between 96.4–95.4 Ma overlain by a post-ridge suite including island-arc related volcanics including boninites formed between 95.4–94.7 Ma (Lasail, V2 unit). The ophiolite obduction process began at 96 Ma with subduction of Triassic–Jurassic oceanic crust to depths of > 40 km to form the amphibolite/granulite facies metamorphic sole along an ENE- dipping subduction zone. U-Pb ages of partial melts in the sole amphibolites (95.6– 94.5 Ma) overlap precisely in age with the ophiolite crustal sequence, implying that subduction was occurring at the same time as the ophiolite was forming. The ophiolite, together with the underlying Haybi and Hawasina thrust sheets, were thrust southwest on top of the Permian–Mesozoic shelf carbonate sequence during the Late Cenomanian–Campanian. -
A Thermal Maturity Analysis of the Effective Cretaceous Petroleum System in the Southern Persian Gulf Basin
Petroleum Engineering Iranian Journal of Oil & Gas Science and Technology, Vol. 6 (2017), No. 4, pp. 01-17 http://ijogst.put.ac.ir A Thermal Maturity Analysis of the Effective Cretaceous Petroleum System in the Southern Persian Gulf Basin Majid Alipour1, Bahram Alizadeh1,2*, and Ali Chehrazi3 1 Ph.D. Candidate, Department of Geology, Faculty of Earth Sciences, Shahid Chamran University, Ahvaz, Iran 2 Professor, Petroleum Geology and Geochemistry Research Center (PGGRC), Shahid Chamran University, Ahvaz, Iran 3 Assisstant Professor, Research Institute of Petroleum Industry (RIPI), Tehran, Iran Received: October 28, 2016; revised: May 15, 2017; accepted: May 22, 2017 Abstract Commercial hydrocarbon discoveries in the Cretaceous of the southern Persian Gulf basin provide direct evidence that there is an effective petroleum system associated with the Cretaceous series. The revised models of thermal maturity in this region are needed to investigate lateral and stratigraphic variations of thermal maturity, which have not so far been addressed in detail for this part of the Persian Gulf. Such thermal maturity models are required to delineate the existing play assessment risks and to predict properties in more deeply buried undrilled sections. This study uses two dimensional basin modeling techniques to reconstruct maturity evolution of the Cenomanian Middle Sarvak source rock, presumably the most likely source for these hydrocarbons. The results indicate that an estimated 900 meter difference in the depth of burial between the southeastern high and the adjacent trough tends to be translated into noticeable variations at both temperature (135 °C versus 162 °C) and vitrinite reflectance (0.91% versus 1.35%). Since the organic matter in the mentioned source rock is of reactive type II, these could cause a shift of about 18 million years in the onset of hydrocarbon generation over respective areas. -
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 � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � -
Saudi Arabia 2019
Saudi Arabia 2019 Saudi Arabia 2019 1 Table of Contents Doing Business in Saudi Arabia ...................................................................................................................................... 5 Market Overview ....................................................................................................................................................... 5 Market Challenges ..................................................................................................................................................... 6 Market Opportunities ................................................................................................................................................ 8 Market Entry Strategy ............................................................................................................................................... 9 Political Environment................................................................................................................................................... 10 Selling US Products & Services .................................................................................................................................... 11 Agents and Distributors ........................................................................................................................................... 11 Establishing an Office ............................................................................................................................................. -
Oman: Politics, Security, and U.S
Oman: Politics, Security, and U.S. Policy Updated May 19, 2021 Congressional Research Service https://crsreports.congress.gov RS21534 SUMMARY RS21534 Oman: Politics, Security, and U.S. Policy May 19, 2021 The Sultanate of Oman has been a strategic partner of the United States since 1980, when it became the first Persian Gulf state to sign a formal accord permitting the U.S. military to use its Kenneth Katzman facilities. Oman has hosted U.S. forces during every U.S. military operation in the region since Specialist in Middle then, and it is a partner in U.S. efforts to counter terrorist groups and other regional threats. In Eastern Affairs January 2020, Oman’s longtime leader, Sultan Qaboos bin Sa’id Al Said, passed away and was succeeded by Haythim bin Tariq Al Said, a cousin selected by Oman’s royal family immediately upon Qaboos’s death. Sultan Haythim espouses policies similar to those of Qaboos and has not altered U.S.-Oman ties or Oman’s regional policies. During Qaboos’s reign (1970-2020), Oman generally avoided joining other countries in the Gulf Cooperation Council (GCC: Saudi Arabia, Kuwait, United Arab Emirates , Bahrain, Qatar, and Oman) in regional military interventions, instead seeking to mediate their resolution. Oman joined but did not contribute forces to the U.S.-led coalition against the Islamic State organization, nor did it arm groups fighting Syrian President Bashar Al Asad’s regime. It opposed the June 2017 Saudi/UAE- led isolation of Qatar and had urged resolution of that rift before its resolution in January 2021. -
Africa-Arabia-Eurasia Plate Interactions and Implications for the Dynamics of Mediterranean Subduction and Red Sea Rifting
This page added by the GeoPRISMS office. Africa-Arabia-Eurasia plate interactions and implications for the dynamics of Mediterranean subduction and Red Sea rifting Authors: R. Reilinger, B. Hager, L. Royden, C. Burchfiel, R. Van der Hilst Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA USA, [email protected], Tel: (617)253 -7860 This page added by the GeoPRISMS office. Our proposed GeoPRISMS Initiative is based on the premise that understanding the mechanics of plate motions (i.e., the force balance on the plates) is necessary to develop realistic models for plate interactions, including processes at subduction and extensional (rifting) plate boundaries. Important advances are being made with new geologic and geophysical techniques and observations that are providing fundamental insights into the dynamics of these plate tectonic processes. Our proposed research addresses directly the following questions identified in the GeoPRISMS SCD Draft Science Plan: 4.2 (How does deformation across the subduction plate boundary evolve in space and time, through the seismic cycle and beyond?), 4.6 (What are the physical and chemical conditions that control subduction zone initiation and the development of mature arc systems?), and 4.7 (What are the critical feedbacks between surface processes and subduction zone mechanics and dynamics?). It has long been recognized that the Greater Mediterranean region provides a natural laboratory to study a wide range of geodynamic processes (Figure 1) including ocean subduction and continent- continent collision (Hellenic arc, Arabia-Eurasia collision), lithospheric delamination (E Turkey High Plateau, Alboran Sea/High Atlas), back-arc extension (Mediterranean basins, including Alboran, Central Mediterranean, Aegean), “escape” tectonics and associated continental transform faulting (Anatolia, North and East Anatolian faults), and active continental and ocean rifting (East African and northern Red Sea rifting, central Red Sea and Gulf of Aden young ocean rifting). -
Pacific Petroleum Eology
Pacific Petroleum Geology NEWSLETTER Pacific Section • American Association of Petroleum Geologists September & October• 2010 School of Rock Ridge Basin CONTENTS 2010-2011 OFF I C E RS EV E RY ISSU E President Cynthia Huggins 661.665.5074 [email protected] 4 Message from the President • C. Huggins President-Elect John Minch 805.898.9200 6 Editor’s Corner • E. Washburn [email protected] Vice President Jeff Gartland 7 PS-AAPG News 661.869.8204 [email protected] 13 Publications Secretary Tony Reid 661.412.5467 17 Member Society News [email protected] Treasurer 2009-2011 Cheryl Blume TH I S ISSU E 661.864.4722 [email protected] 8 Sharktooth Hill Fossil Fund • K. Hancharick Treasurer 2010-2012 Jana McIntyre 661.869.8231 [email protected] 10 AAPG Young Professionals • J. Allen Past President Scott Hector 11 Serpentine: The Rest of the Story • Mel 707.974.6402 [email protected] Erskine Editor-in-Chief Ed Washburn 661.654.7182 [email protected] ST AFF Web Master Bob Countryman 661.589.8580 [email protected] Membership Chair Brian Church 661.654.7863 [email protected] Publications Chair Larry Knauer 661.392.2471 [email protected] [email protected] Advisory Council Representative Kurt Neher 661.412.5203 [email protected] Cover photo of Ridge Basin outcrop courtesy Jonathan Allen Page 3 Pacific Petroleum Geologist Newsletter September & October • 2010 MESSAGE FRO M THE PRESIDENT CYNTHIA HUGGINS Do you know what Marilyn Bachman, Mike Fillipow, Peggy Lubchenco, and Jane Justus Frazier have in common? They were all recipients of the Teacher of the Year Award from AAPG, and they all came from the Pacific Section! Of the 13 recipients of this award, four have been from PSAAPG.