DOCSLIB.ORG

Eurasia Asia & Oceania

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Segment Overview Asia & Eurasia Oceania u p. 28 u p. 20 Number of countries 7 4 1,551 ,296 1 1,245 1,218 1 16 14 Number of projects 1 3 In production 2 43 1 1 6 Under development 10 Preparation for development Under exploration (oil and gas reservoirs confirmed) Under exploration Other 466 Production/Reserves 367 Proved reserves (million boe) 214 201 195 210 207 191 Net production (thousand boed) 179 197 190 188 167 166 28 27 27 26 25 25 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 485,275 485,069 483,187 406,828 409,776 / 352,383 Net sales 299,599 281,623 Operating income 264,849 235,814 Net sales (¥ million) 191,070 178,225 Operating income (¥ million) 96,341 94,050 85,541 84,325 73,574 68,319 47,076 41,752 42,601 39,769 36,461 32,228 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 018 INPEX CORPORATION Annual Report 2015 Middle East Americas Japan & Africa u p. 32 u p. 36 u p. 30 6 7 1 Minami-Nagaoka 1 2 Gas Field 1 Naoetsu LNG 3 Terminal 9 7 1 16 10 Natural gas pipeline network (Approx. 1,400 km) etc. 783 857 636 4 Project Overview Project 583 518 505 174 168 169 158 163 155 138 135 132 130 126 117 74 68 65 40 36 30 29 30 27 28 20 25 25 21 21 21 17 18 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 524,528 520,835 500,033 621,513 421,184 357,343 354,136 350,735 333,213 303,819 243,113 205,572 129,522 120,268 118,937 ) 113,662 104,525 93,959 32,555 28,568 25,959 22,771 24,607 16,692 16,693 12,673 11,435 13,351 15,303 5,945 5,525 (7,646) (3,035) 1,028 (6,089) (5,518) ( 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 INPEX CORPORATION Annual Report 2015 019 Project Overview by Region Asia & Oceania In the Asia and Oceania region, INPEX holds participating interests in the Offshore Mahakam Block in Indonesia, which is contributing significantly to earnings, and the large-scale Ichthys and Abadi LNG projects, where development and preparatory development activities are under way. The Company is also actively advancing more than 20 exploration projects with growth potential across the region. 020 INPEX CORPORATION Annual Report 2015 1 Offshore Mahakam Block and Attaka Unit INPEX entered into a production shar- This venture subsequently made a series The Offshore Mahakam Block has ing contract (PSC) with the Indonesian of discoveries in the Bekapai (oil), Handil begun to see output decline after more Government in October 1966, at that (oil), Tambora (oil and gas), Tunu (gas), than 40 years of production. In 2012, time acquiring a 100% interest in the Peciko (gas), Sisi and Nubi (gas), as well impediments at production wells led to Offshore Mahakam Block. The Attaka as the South Mahakam (gas), fields, each a large drop in output, in addition to nat- Unit was established in April 1970 of which has continued to produce crude ural attrition. Thereafter, successful steps through the unitization of part of the oil and natural gas. The crude oil and con- were taken to control the decline in pro- adjacent blocks owned by INPEX and densate produced from these fields are duction. In addition to measures aimed Unocal (now Chevron), with each com- shipped mainly to oil refineries and power at counteracting sand problems, INPEX pany taking a 50% interest. Production companies in Japan by tanker from the accelerated the pace at which it under- of crude oil and natural gas has contin- Santan and Senipah terminals. Most of took development well drilling. Produc- ued since 1972. INPEX farmed out 50% the natural gas is supplied to the Bontang tion volumes have remained stable since of its interest in the Offshore Mahakam LNG Plant, and then shipped as LNG to 2013. Block to CFP (now TOTAL) in July 1970. customers in Japan and elsewhere. Contract area Project status Venture company Interest owned (block) (production on the basis of all fields and average rate of FY2014) (established) (*Operator) Crude oil: 72 Mbbld Offshore Mahakam INPEX CORPORATION INPEX 50% TOTAL* 50% In production Natural gas: 1,257 MMcf/d (February 21, 1966) Attaka Unit LPG: 11 Mbbld INPEX 50% Chevron* 50% Bontang LNG Plant Attaka Unit Santan Terminal Attaka Field Badak Field Nilam Field Tunu Field Tambora Field Sisi Field 4 Handil Field Overview Project Nubi Field Senipah Terminal Bekapai Field Balikpapan Peciko Field Offshore INDONESIA Mahakam Block South Mahakam Field Gas field Oil field Oil and gas field 1 2 1: Compression unit 2: Production facility INPEX CORPORATION Annual Report 2015 021 2 South Natuna Sea Block B FPSO vessel In July 1977, INPEX acquired a 17.5% duction, storage and offloading (FPSO) Natuna Sea interest in the South Natuna Sea Block B in system. Production of crude oil and con- South Natuna Sea North Belut Block B Indonesia. Later, in January 1994, INPEX densate began in December 2004, with Belida Kerisi Bawal increased its total interest in the block to LPG production commencing in April 35% with the purchase of an additional 2007. After 2006 at this same block, pro- interest. Crude oil production began in duction began at the Hiu Gas, Kerisi Oil South Belut Natuna Island 1979, and supplies of natural gas to Sin- and Gas, North Belut Gas and Bawal Gas Hiu gapore via Indonesia’s first international fields. Most recently, production com- Sembilang Belanak pipeline commenced in 2001. Additional menced at the South Belut Gas Field in Gas field Oil field Oil and gas field deliveries of natural gas from this pipeline April 2014. to Malaysia started in 2002. These supply milestones contributed to the extension Project status Contract area Venture company Interest owned (production on the basis of all fields and of the PSC covering the block until 2028. (block) (established) (*Operator) average rate of FY2014) Production operations in the Belanak Crude oil: 27 Mbbld INPEX Natuna 35% South Natuna INPEX Natuna, Ltd. oil and gas field, which is part of South In production Natural gas: 354 MMcf/d ConocoPhillips* 40% Sea B (September 1, 1978) Natuna, utilize a world-class floating pro- LPG: 12 Mbbld Chevron 25% 3 Sebuku Block Ruby Gas Field Fertilizer plant In September 2010, INPEX obtained a Bontang LNG Plant Attaka Field 15% interest in the Sebuku Block off the Santan Terminal shore of South Makassar, Indonesia. There- Tunu Field Senipah Terminal after, work began to develop the Ruby Peciko Field Gas Field in the block, and production Balikpapan of natural gas followed in October 2013. South Mahakam Field Kalimantan The natural gas produced here is trans- ported from offshore production facilities Makassar Strait via undersea pipeline to onshore storage INDONESIA facilities that receive products from the Sebuku Block Sulaewesi Offshore Mahakam Block. The natural gas Gas field is then mainly sent via inland pipeline to a Ruby Gas Field Oil field fertilizer plant in East Kalimantan. Offshore production facility in the Ruby Gas Field Contract area Project status Venture company Interest owned (block) (production on the basis of all fields and average rate of FY2014) (established) (*Operator) INPEX South Makassar, Ltd. INPEX South Makassar 15％ Sebuku In production (Natural gas: 73 MMcf/d) (May 17, 2010) PEARL OIL (Sebuku) Ltd.* 70% TOTAL 15% 022 INPEX CORPORATION Annual Report 2015 4 Abadi LNG Project INPEX acquired a 100% interest in the work. Meanwhile, INPEX also has studied Masela Block in November 1998 through the feasibility of full field development, Tanimbar Island an open bid conducted by the Indone- drilling three appraisal wells between INDONESIA sian government and subsequently went 2013 and 2014 with the aim of expand- Abadi Gas Field Arafura Sea about exploratory activities as Operator, ing the volume of recoverable reserves. discovering the Abadi Gas Field through Evaluations of these wells resulted in the the first exploratory well drilled in 2000. confirmation of a substantially greater AUSTRALIA The company subsequently drilled two volume of natural gas reserves, which Timor Sea appraisal wells in 2002 and four in 2007– was certified by Indonesian authorities. 2008, all of which confirmed the pres- Taking those into consideration, INPEX is ence of gas and condensate reservoirs. studying ways to optimize development Darwin In December 2010, Indonesian authori- plans centered on a large-scale FLNG Gas field ties approved the initial plan of develop- and is currently in discussions with the ment (POD-1) deploying a floating LNG Indonesian government. (FLNG) plant with an annual processing capacity of 2.5 million tons, and from Contract area (block) Project status Venture company (established) Interest owned (*Operator) November 2012 to November 2014, Preparation for INPEX Masela, Ltd. INPEX Masela* 65% INPEX undertook SURF (subsea, umbil- Masela development (December 2, 1998) Shell 35％ ical, riser and flowline) and FLNG FEED 4 Project Overview Project 1 2 3 1: Drillship for the Abadi LNG Project 2: Production test 3: Floating LNG (rendering) INPEX CORPORATION Annual Report 2015 023 5 The Ichthys LNG Project and Surrounding Blocks Project Overview ensuing period, INPEX has continued to jetties to accommodate module ship- In 1997, INPEX placed an open tender engage in engineering, equipment pro- ment. Currently, pipe-laying work for the bid to acquire the petroleum exploration curement and construction work activ- 889-km-long gas export pipeline (GEP) permit WA-285-P located approximately ities with respect to both onshore and that will connect the Ichthys gas-con- 200 km northwest of Western Australia’s offshore production facilities.
Recommended publications
  • Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra

    Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra

    Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473.
  • From Africa to Eurasia * Early Dispersals Ofer Bar-Yosef! *, A

    From Africa to Eurasia * Early Dispersals Ofer Bar-Yosef! *, A

    Quaternary International 75 (2001) 19}28 From Africa to Eurasia * early dispersals Ofer Bar-Yosef! *, A. Belfer-Cohen" !Department of Anthropology, Peabody Museum, Harvard University, Cambridge, MA 02138, USA "Institute of Archaeology, Hebrew University, Jerusalem 91905, Israel Abstract The dispersals of early hominins in the late Pliocene or early Pleistocene into Eurasia were essentially sporadic. Little geographic and temporal continuity is observed between the various dated archaeological contexts, and the lithic assemblages do not demonstrate a techno-morphological continuity. The archaeological evidence from 1.8 to 0.7 Ma indicates at least three waves of early migrations. The earliest sortie involved bearers of core-chopper industries sometime around 1.7}1.6 Ma. Early Acheulean producers followed possibly around 1.4 Ma. The third wave occurred sometime around 0.8 Ma, and is represented by Acheulean groups who manufactured numerous #ake cleavers. The geographic scope of each of these waves is not yet well known.The reasons for &why' early humans dispersed from Africa into Eurasia include the &push' of environmental change and relative &demographic pressure', as well as the opening of new niches. Humans may have gained their meat supplies either from carcasses or through active predation. The archaeological and fossil records demonstrate that Homo erectus was a successful species, and like other successful species it enlarged its geographic distribution at all costs. Even if the trigger for the initial dispersal of Homo erectus remains unknown or controversial, the success of the hominid occupation of the Eurasian habitats was not primarily facilitated by the availability of food, or the human #exibility in food procuring techniques, but by the absence of the zoonotic diseases that plagued and constrained hominins in their African &cradle of evolution'.
  • No. 1 Demography and Health in Eastern Europe and Eurasia

    No. 1 Demography and Health in Eastern Europe and Eurasia

    Working Paper Series on the Transition Countries No. 1 DEMOGRAPHY AND HEALTH IN EASTERN EUROPE AND EURASIA Ayo Heinegg Robyn Melzig James Pickett and Ron Sprout June 2005 Program Office Bureau for Europe & Eurasia U.S. Agency for International Development 1 Demography and Health in Eastern Europe and Eurasia Ayo Heinegg Academy for Educational Development Email: [email protected] Robyn Melzig U.S. Agency for International Development, Washington DC Email: [email protected] James Pickett U.S. Agency for International Development, Washington DC Email: [email protected] Ron Sprout U.S. Agency for International Development, Washington DC Email: [email protected] Abstract: Eastern Europe and Eurasia is the only region worldwide experiencing a contraction in population, which stems from both a natural decrease in the population (i.e., crude death rates exceeding crude birth rates) and emigration. The highest crude death rates in the world are found among the transition countries; so too the lowest fertility rates. This study analyzes these trends and attempts to assess some of the underlying health factors behind them. The report also examines the evidence regarding migration patterns, both political aspects (including trends in refugees and internally displaced persons) and economic aspects (including remittances, urbanization, and brain drain). 2 USAID/E&E/PO Working Paper Series on the Transition Countries September 2006 No.1 Demography and Health (June 2005) No.2 Education (October 2005) No.3 Economic Reforms, Democracy, and Growth (November 2005) No.4 Monitoring Country Progress in 2006 (September 2006) No.5 Domestic Disparities (forthcoming) No.6 Labor Markets (forthcoming) No.7 Global Economic Integration (forthcoming) The findings, interpretations, and conclusions expressed in these working papers are entirely those of the authors.
  • Russia and Eurasia Steven Pifer

    Russia and Eurasia Steven Pifer

    14 Russia and Eurasia Steven Pifer Russia for the past 4 years has been on an economic roll fueled by high energy prices. The Kremlin in parallel has pursued an increasingly assertive foreign policy, raising the prospect of a more contentious Russia that will challenge U.S. interests in the former Soviet space, Europe, and elsewhere. The challenges posed by a more assertive Russia will command greater time and attention from U.S. national security planners. It is not only a resurgent Russia that could test the United States in coming years, however. A frail, unstable Russian state is not in the U.S. interest. Russian weakness raises less obvious, but nevertheless serious, possible challenges. Demographic, societal, and economic trends within Russia have the potential, particularly in combination, to create strategic shocks over the next 10 to 30 years that would have major implications for U.S. national security interests. This chapter examines those trends and potential shocks and outlines implications for U.S. national security. The strategic shocks that trends within Russia could combine to produce include collapse of the Russian state, expansion to take in more ethnic Russians, revolution (leading to a lurch toward democracy or, more likely, to the right), playing the energy card, and a military/technical surprise. While these shocks each have a very low likelihood, any of them would pose critical implications and challenges for key U.S. security interests. This chapter also looks at possible shocks elsewhere in the former Soviet space: Islamic revolution in a Central Asian state and Georgian-Russian military conflict, with the latter being the most likely shock of those addressed.
  • Eurasia Foundation Network

    Eurasia Foundation Network

    Engaging Citizens Empowering Communities Eurasia2009 Network Foundation Yearbook Engaging Citizens, Empowering Communities Eurasia Foundation Network EURASIA FOUNDATION OF CENTRAL ASIA TABLE OF CONTENTS Advisory Council, Board of Trustees.....................1 2009 Letter from the Chair and President..............................2 The Eurasia Foundation Network......................................3 Yearbook Overview.....................................4 New Eurasia Foundation.................................5 Eurasia Foundation of Central Asia..........................6 Eurasia Partnership Foundation.................................7 East Europe Foundation.................................8 Youth Engagement...................9 Local Economic Development...........................11 Public Policy and The Eurasia Foundation Network comprises New Eurasia Foundation (Russia), Eurasia Foundation of Central Asia, Eurasia Partnership InstitutionFoundation Building.................13 (Caucasus), East Europe Foundation (Ukraine, Belarus, Moldova) and Eurasia Foundation (United States). Since 1993, Eurasia Foundation and the network have invested more than $360 million in local and cross-border projects to promote civic and economic inclusion throughout the Eurasia region.Independent Media.................15 For more information about the Eurasia Foundation Network, please visit http://www.eurasia.org/ Cross-Border Programs ........17 Eurasia Foundation Financials..................................19 EAST EUROPE EURASIA FOUNDATION EFFOUNDATION Network
  • 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

    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).
  • The Role of Eurasia in a Multi-Polar World

    The Role of Eurasia in a Multi-Polar World

    THE ROLE OF EURASIA IN A MULTI-POLAR WORLD AHMET EVIN MEGAN GISCLON Istanbul Policy Center Bankalar Caddesi No: 2 Minerva Han 34420 Karaköy, İstanbul TURKEY +90 212 292 49 39 +90 212 292 49 57 @ [email protected] ISBN: 978-605-2095-47-8 w ipc.sabanciuniv.edu THE ROLE OF EURASIA IN A MULTI-POLAR WORLD AHMET EVIN MEGAN GISCLON March 2019 Ahmet Evin is a senior scholar at Istanbul Policy Center and professor emeritus at Sabanci University. Megan Gisclon is managing editor and researcher at Istanbul Policy Center. About Istanbul Policy Center Istanbul Policy Center is an independent policy research institute with global outreach. Our mission is to foster academic research in social sciences and its application to policy making. We are firmly committed to providing decision makers, opinion leaders, academics, and the general public with innovative and objective analyses in key domestic and foreign policy issues. IPC has expertise in a wide range of areas, including—but not exhaustive to—Turkey-EU-U.S. relations, conflict resolution, education, climate change, current trends of political and social transformation in Turkey, as well as the impact of civil society and local governance on this metamorphosis. PREFACE As part of its Observatory Program, Istanbul Policy of gravity of global trade, and more recently, of the Center (IPC), in cooperation with the German Council centrifugal forces acting upon the Western world, on Foreign Relations (Deutsche Gesellschaft für the present conference was organized to address the Auswärtige Politik, DGAP), organized a conference increasing number of questions regarding Eurasia: the on “The Role of Eurasia in a Multi-Polar World.” This vast landmass between Europe and China, dominated one-day roundtable took place on December 6, 2017 at since the middle of the nineteenth century by Russia, DGAP’s Berlin office.
  • Arctic Report Card 2018 Effects of Persistent Arctic Warming Continue to Mount

    Arctic Report Card 2018 Effects of Persistent Arctic Warming Continue to Mount

    Arctic Report Card 2018 Effects of persistent Arctic warming continue to mount 2018 Headlines 2018 Headlines Video Executive Summary Effects of persistent Arctic warming continue Contacts to mount Vital Signs Surface Air Temperature Continued warming of the Arctic atmosphere Terrestrial Snow Cover and ocean are driving broad change in the Greenland Ice Sheet environmental system in predicted and, also, Sea Ice unexpected ways. New emerging threats Sea Surface Temperature are taking form and highlighting the level of Arctic Ocean Primary uncertainty in the breadth of environmental Productivity change that is to come. Tundra Greenness Other Indicators River Discharge Highlights Lake Ice • Surface air temperatures in the Arctic continued to warm at twice the rate relative to the rest of the globe. Arc- Migratory Tundra Caribou tic air temperatures for the past five years (2014-18) have exceeded all previous records since 1900. and Wild Reindeer • In the terrestrial system, atmospheric warming continued to drive broad, long-term trends in declining Frostbites terrestrial snow cover, melting of theGreenland Ice Sheet and lake ice, increasing summertime Arcticriver discharge, and the expansion and greening of Arctic tundravegetation . Clarity and Clouds • Despite increase of vegetation available for grazing, herd populations of caribou and wild reindeer across the Harmful Algal Blooms in the Arctic tundra have declined by nearly 50% over the last two decades. Arctic • In 2018 Arcticsea ice remained younger, thinner, and covered less area than in the past. The 12 lowest extents in Microplastics in the Marine the satellite record have occurred in the last 12 years. Realms of the Arctic • Pan-Arctic observations suggest a long-term decline in coastal landfast sea ice since measurements began in the Landfast Sea Ice in a 1970s, affecting this important platform for hunting, traveling, and coastal protection for local communities.
  • Northern Large Marine Domain

    Northern Large Marine Domain

    Collation and Analysis of Oceanographic Datasets for National Marine Bioregionalisation: The Northern Large Marine Domain. A report to the Australian Government, National Oceans Office. May 2005 CSIRO Marine Research Peter Rothlisberg Scott Condie Donna Hayes Brian Griffiths Steve Edgar Jeff Dunn Cover Image designed by Vincent Lyne CSIRO Marine Researchi Cover Design Lea Crosswell and Louise Bell CSIRO Marine Research Collation and Analysis of Oceanographic Datasets – The Northern Large Marine Domain Contents Contents...........................................................................................................................................i List of Figures.................................................................................................................................ii 1. Summary................................................................................................................................1 2. Project Objectives..................................................................................................................2 3. Background............................................................................................................................2 4. Data Storage and Metadata....................................................................................................2 5 Setting for the Northern Large Marine Domain ....................................................................3 5.1 Geomorphology..............................................................................................................4
  • Seismic Anisotropy and the Mantle Dynamics Beneath the Arabian Plate

    Seismic Anisotropy and the Mantle Dynamics Beneath the Arabian Plate

    Scholars' Mine Doctoral Dissertations Student Theses and Dissertations Fall 2018 Seismic anisotropy and the mantle dynamics beneath the Arabian plate Saleh Ismail Hassan Qaysi Follow this and additional works at: https://scholarsmine.mst.edu/doctoral_dissertations Part of the Geophysics and Seismology Commons Department: Geosciences and Geological and Petroleum Engineering Recommended Citation Qaysi, Saleh Ismail Hassan, "Seismic anisotropy and the mantle dynamics beneath the Arabian plate" (2018). Doctoral Dissertations. 2727. https://scholarsmine.mst.edu/doctoral_dissertations/2727 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. SEISMIC ANISOTROPY AND THE MANTLE DYNAMICS BENEATH THE ARABIAN PLATE by SALEH ISMAIL HASSAN QAYSI A DISSERTATION Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree DOCTOR OF PHILOSOPHY in GEOLOGY AND GEOPHYSICS 2018 Approved by: Kelly Liu, Advisor Stephen Gao Neil L. Anderson Ralph Flori Jr Saad Mogren 2018 Saleh Ismail Hassan Qaysi All Rights Reserve iii PUBLICATION DISSERTATION OPTION This dissertation consists of two articles formatted using the publication option. Paper I, the pages from 3 – 19 were accepted for publication in the Seismological Research Letter on December 19, 2018 under number (SRL-D-18-00144_R1). Paper II, the pages from 20 – 56 are in a preparation to be submitted to a scientific journal. iv ABSTRACT We investigate mantle seismic azimuthal anisotropy and deformation beneath the Arabian Plate and adjacent areas using data from 182 broadband seismic stations which include 157 stations managed by the Saudi Geological Survey.
  • Autumn 2014 2 Consecration in Canterbury

    Autumn 2014 2 Consecration in Canterbury

    THE E UROP E AN A NGLICAN C ANT E RBURY C ONS E CRATION A PPLAUS E F OR O UR N E W B ISHOP M OR E T HAN A S INGL E T OPIC G E N E RAL S YNOD R E PORT P RI E STLY T RIO O RDINATIONS I N C OLOGN E A G RI M M em ORIAL A UTU M N 1 9 1 4 R emem B E R E D S WISS S KI S E RVIC E 1 5 0 Y E ARS W ITN E SS europe.anglican.org No.63 AUTUMN 2014 2 CONSECRATION IN CANTERBURY THE E UROP E AN E UROP E AN , E CU me NICAL AND E NCOURAGING A NGLICA N B ISHOP R OB E RT ’S The Bishop of Gibraltar in Europe The Rt Rev Robert Innes F IRST ST E PS The Suffragan Bishop in Europe The Rt Rev David Hamid Postal address: Diocesan Office Tel: +44 (0) 207 898 1160 Email: [email protected] The Diocesan Office 14 Tufton Street, London, SW1P 3QZ Tel: +44 (0) 207 898 1155 Fax: +44 (0) 207 898 1166 Email: [email protected] Diocesan Secretary Mr Adrian Mumford Appointments Secretary Miss Catherine Jackson Finance Secretary Mr Nick Wraight Diocesan Website www.europe.anglican.org Editor and Diocesan Communications Officer The Rev Paul Needle and boys voices together, and with the Postal address: Diocesan Office backing of trumpeters they did justice to Email: the old German hymn Praise to the Lord, [email protected] the Almighty, the King of creation.
  • The Tectonic History of the Banda Arcs, Eastern Indonesia: a Review

    The Tectonic History of the Banda Arcs, Eastern Indonesia: a Review

    J. geol. Soc. London, Vol. 136, 1979, pp. 519-527,2 figs. Printed inNorthern Ireland. The tectonic history of the Banda Arcs, eastern Indonesia: a review M. S. Norvick SUMMARY: The Banda Sea is underlain by a small marginal oceanic plate, which is believed to have formed during the early Tertiary. Unlike other marginal seas to the N, the spreading of the Banda platelet was restricted by surrounding continental blocks. Its present complexity is a result of late Miocene-earlyPliocene collision and obduction of theBanda Sea island arc system over the leading edge of the Australian-lrian continental plate. Transcurrent faultingon the northern limb of the collision zone may have accentuated curvature of the arc. Subduction and volcanicitv ceased after collision in the Timor and Seram sectors, but are still active at the eastern extremity of the arc. Adouble spiral line of geologicallyvery complex, based on bathymetry (Mammerickx et al. 1976), reg- small, mountainous islands make up the Banda Arcs ional gravity (Vening Meinesz 1954; Chamalaun et al. of eastern Indonesia (Fig. 1). Although onshore out- 1976; Milsom 1977)and earthquake distribution crop information is scattered, and geophysical data on (Hamilton 1974a; Cardwell & Isacks1978). Seismic the deep seas that cover 90% of the area sparse, the lineshave been published across the Timor region tectonic history of the region has stimulated discussion (Branson1974; Beck & Lehner1974; Crostella & formany years, and produced different (sometimes Powell 1975) and the Seram Trough (Audley-Charles conflicting) interpretations. The present review attempts& Carter 1978). Two 1976 oceanographic surveys run to reinterpretto critically thedata and some of by Scripps(‘Indopac’ programme) and CCOP (‘Val- theplate tectonic theories on theevolution of the divia’ cruise) collected valuable seismic refraction and Banda Arcs in the light of recent geological mapping reflection data over the deep water areas (Purdy et al.