Explanatory Notes for the Energy-Resources Map of the Circum-Pacific Region, Pacific Basin Sheet

Total Page:16

File Type:pdf, Size:1020Kb

Explanatory Notes for the Energy-Resources Map of the Circum-Pacific Region, Pacific Basin Sheet 1USGS science fora changing world To Accompany Map CP-50 Explanatory Notes for the Energy-Resources Map of the Circum-Pacific Region, Pacific Basin Sheet By KENNETH J. DRUMMOND, TOMOAKI SUMII, KOJIWAKITA, OS AMU MATSUBAYASHI, KEIZO FUJII, TOMOYUKI MORITANI, W. DAVID PALFREYMAN, MARCELO R. YRIGOYEN, and JOSE CORVALAN D. " I, ____CIRCUM-PACIFIC 2 _____ 1 _____ ______ _____ vCOUN ^1 ENERGY AND MINERAL » i i / RESOURCES 2000 U.S. Department of the Interior U.S. Geological Survey CIRCUM-PACIFIC COUNCIL FOR ENERGY AND MINERAL RESOURCES Michel T. Halbouty, Founder CIRCUM-PACIFIC MAP PROJECT John A. Reinemund, Director George Gryc, General Chairman EXPLANATORY NOTES FOR THE ENERGY-RESOURCES MAP OF THE CIRCUM-PACIFIC REGION PACIFIC BASIN SHEET Scale: 1:17,000,000 By Kenneth J. Drummond, National Energy Board, Calgary, Alberta Tomoaki Sumii, Koji Wakita, Osamu Matsubayashi, Keizo Fujii, and Tomoyuki Moritahi, Geological Survey of Japan, Ibaraki, Japan W. David Palfreyman, Australian Geological Survey Organisation, Canberra, Australia Marcelo R. Yrigoyen, Trend Argentina, S.A., Buenos Aires, Argentina Jose Corvalan D., Servicio Nacional de Geologia y Mineria, Santiago, Chile 2000 Explanatory Notes to Supplement the ENERGY RESOURCES MAP OF THE CIRCUM-PACIFIC REGION PACIFIC BASIN SHEET PETROLEUM RESOURCES Kenneth J. Drummond, National Energy Board, Calgary, Alberta, Canada Marcelo R. Yrigoyen, Trend Argentina S.A., Buenos Aires, Argentina Guillermo P. Salas, Consijo de Recursos Minerales, Mexico, D.F.7 Mexico Tomoaki Sumii, and Hiro'o Natori, Geological Survey of Japan, Tsukuba 305, Japan Masakazu Kato, Japan National Oil Corporation, Tokyo 100, Japan W. David Palfreyman, Australian Geological Survey Organisation, Canberra, Australia COAL DEPOSITS Keizo Fujii, Eiji Inoue, and Masatoshi Sogabe, Geological Survey of Japan, Tsukuba 305, Japan Marcelo R. Yrigoyen, Trend Argentina S.A., Buenos Aires, Argentina W. David Palfreyman, Australian Geological Survey Organisation, Canberra. Australia Gordon H. Wood and William V. Hour, III, U.S. Geological Survey, Reston, Virginia 22092,U.S.A. Paul W. Richards, Valley Center, California 92082, U.S.A. GEOTHERMAL RESOURCES Marcelo R. Yrigoyen, Trend Argentina S.A., Buenos Aires, Argentina Theresa R. Swint-Iki, U.S. Geological Survey, Menlo Park, California U.S.A. Osamu Matsubayashi, Geological Survey of Japan, Tsukuba 305, Japan W. David Palfreyman, Australian Geological Survey Organisation, Canberra. Australia GEOLOGIC BACKGROUND Kenneth J. Drummond, National Energy Board, Calgary, Alberta, Canada Jose Corvalan D., Servicio Nacional de Geologia y Mineria, Santiago, Chile Marcelo R. Yrigoyen, Trend Argentina S.A., Buenos Aires, Argentina Koji Wakita and Tomoaki Sumii, Geological Survey of Japan, Tsukuba 305, Japan H. Frederick Doutch and W. David Palfreyman, Australian Geological Survey Organisation, Canberra, Australia Map compilation coordinated by George Gryc, Circum-Pacific Map Project General Chairman, U.S. Geological Survey, Menlo Park, California 94025, U.S.A 11 CONTENTS Introduction 1 Circum-Pacific Map Project 1 Energy-Resources Map of the Pacific Basin Sheet 1 Background Information 2 Land Areas 2 Ocean areas 4 Geologic setting 4 Tectonic setting 5 Energy resources 7 Oil and natural gas 7 Sedimentary basins of Northeast Quadrant 7 Offshore Pacific Coast of the United States 9 Onshore Southern California basins 10 Middle America Marginal-Trough Basin 10 Oil sand 14 Oil shale 14 Coal 15 Geothermal resources 17 References cited and additional sources of data (from Explanatory Notes accompanying Quadrant Maps) 21 Northeast Quadrant 21 Southeast Quadrant 24 Northwest Quadrant 27 Southwest Quadrant 34 Additional Sources of Data 34 Figures 1-24 37-64 Tables 1-20 65-106 Appendix I. Conversion factors 107 Appendix II. List of abbreviations used 107 Appendix III. Glossary 107 Appendix IV. Summarized A.S.T.M. classification of coals by rank 109 111 INTRODUCTION 951, Menlo Park, California 94025, U.S.A. The project has been overseen from its inception by John A. CIRCUM-PACIFIC MAP PROJECT Reinemund, Director of the project since 1982. The framework for the Circum-Pacific Map Project The Circum-Pacific Map Project (CPMP) is a coop­ was developed in 1973 by a specially convened group of erative international effort designed to show the relation­ 12 North American geoscientists meeting in California. ship of known energy and mineral resources to the major The project was officially launched at the First Circum- geologic features of the Pacific basin and surrounding Pacific Conference on Energy and Mineral Resources, continental areas. Available geologic, mineral, and en­ which met in Honolulu, Hawaii, in August 1974. Spon­ ergy-resource data are being complemented by new, sors of the conference were the American Association of project-developed data sets such as magnetic lineations, Petroleum Geologists (AAPG), Pacific Science Associa­ seafloor mineral deposits, and seafloor sediment. Earth tion (PSA), and the Coordinating Committee for Offshore scientists representing some 180 organizations from more Prospecting for Mineral Resources in Offshore Asian than 40 Pacific-region countries are involved in this work. Areas (CCOP). The Circum-Pacific Map Project oper­ Six overlapping equal-area regional maps at a scale of ates as an activity of the Circum-Pacific Council for En­ 1:10,000,000 form the cartographic base for the project: the ergy and Mineral Resources, a nonprofit organization that four Circum-Pacific Quadrants (Northwest, Southwest, promotes cooperation among Circum-Pacific countries Southeast, and Northeast), and the Antarctic and Arctic in the study of energy and mineral resources of the Pa­ Sheets. There is also a Pacific Basin Sheet at a scale of cific basin. Founded by Michel T. Halbouty in 1972, the 1:17,000,000. The published map series include the Base Council also sponsors quadrennial conferences, topical Map Series and the Geographic Series (published from 1977 symposia, scientific training seminars, and the Earth Sci­ to 1990), the Plate-Tectonic Series (published from 1981 to ence Series of publications. 1992), the Geodynamic Series (published from 1984 to 1990), and the Geologic Series (published from 1984 to ENERGY-RESOURCES MAP OF THE 2000); all include six map sheets. The thematic map series PACIFIC BASIN SHEET in the process of completing publication include Mineral- Resources and Energy-Resources Maps. Altogether, 60 map The Energy-Resources Map of the Circum-Pacific sheets are planned. Region, Basin Sheet is a compilation at a scale of The maps are prepared cooperatively by the Circum- 1:17,000,000 of a series of four overlapping 1:10,000,000- Pacific Council for Energy and Mineral Resources and scale map sheets. The maps in the 1:10,000,000 series the U.S. Geological Survey and are available from USGS, includes the Northeast Quadrant, Southeast Quadrant, Information Services, Box 25286, Federal Center, Den­ Northwest Quadrant, and the Southwest Quadrant, and ver, Colorado 80225, U.S.A. Maps published prior to mid- an Arctic Sheet. 1990 are available from Dr. H. Gary Greene, Circum- Information depicted on the Energy-Resources Map Pacific Council for Energy and Mineral Resources, Moss of the Circum-Pacific Region, Basin Sheet includes a Landing Marine Laboratory, MLML, Box 450, Moss generalized geologic background, oil and gas fields, oil Landing, California 95039-0450, U.S.A sands, oil shale, coal deposits, geothermal energy sites, The Circum-Pacific Map Project is organized under hot springs, onshore basin isopachs, and sediment isop- six panels of geoscientists representing national earth- achs in ocean areas. science organizations, universities, and natural-resource The geologic background for the Energy-Resources companies. The six panels correspond to the basic map Map shows the relevance of the "economic basement" to areas. Current panel chairs are Kenneth J. Drummond the sedimentary basin areas. Depicted in a generalized (Northeast Quadrant), Tomoyuki Moritani (Northwest format are Precambrian basement, igneous intrusives, Quadrant), George W. Moore (Arctic Region), lan W.D. volcanic cover, and deformed sedimentary fold belts. Dalziel (Antarctic Region), vacant (Southwest Quadrant), Bathymetry and sediment isopachs comprise the back­ vacant, (Southeast Quadrant). Jose Corvalan D., chaired ground for the oceanic areas. the Southeast Quadrant Panel from its inception in 1974 Active plate boundaries shown in red are taken from to his death in 1996; the Panel completed compilations the Plate-Tectonic Map of the Circum-Pacific Region of all eight topical maps of that quadrant. (Moore, 1981). Spreading axes are depicted as lines of Project coordination and final cartography are being uniform width (1 mm) rather than by lines of varying carried out by the U.S. Geological Survey, under the di­ width to represent spreading rates as is done on the Plate- rection of Circum-Pacific Map Project General Chair­ Tectonic Maps. man George Gryc of Menlo Park, California. Project The purpose of this report is to supplement the En­ headquarters are located at 345 Middlefield Road, MS ergy-Resources Map of the Circum-Pacific Region, Ba- sin Sheet with additional data, explanations, and ref­ Drummond, Mobil Oil of Canada, Calgary, Alberta, erences that could not be depicted on the face of the Canada, was used. Other principal investigators and map. The notes for the Basin Sheet have been excerpted sources of data are indicated in the references sections from the earlier published Explanatory
Recommended publications
  • Andinismo: Desafío Para La Prensa Nacional Memoria Para Optar Al Título De Periodista
    UNIVERSIDAD NACIONAL 11111111111111�ñi�íll1i1i1l1lm1111111111111 35612000064981. UNIVERSIDADa ANDRES BELLO UNIVERSIDAD ANDRÉS BELLO FACULTAD DE HUMANIDADES Y EDUCACIÓN ESCUELA DE PERIODISMO ANDINISMO: DESAFÍO PARA LA PRENSA NACIONAL MEMORIA PARA OPTAR AL TÍTULO DE PERIODISTA ALUMNO: CARLA BERTOSSI ARRIBADA PROFESOR GUÍA: SEBASTIANO BERTOLONE GALLETINI SANTIAGO - CHILE Noviembre, 2004 ÍNDICE Justificacióndel Tema ............................................................................................ 2 ANDINISMO: DESAFÍO PARA LA PRENSA NACIONAL ............................................ 4 Introducción............... ......................................................................................... 5 Capítulo I CARACTERÍSTICAS FÍSICAS DE LOS ANDES ......................................................... 8 1. Geografia de Los Andes 2. El ambientede montaña 3. Cumbres emblemáticas Capítulo II MONTAÑAS, TEMPLO DEL DEPORTE.................................................................. 29 l. Breve historia del andinismo 2. El deporte de montaña 3. Andinismo 4. Organización del andinismo en Chile Capítulo m TÉCNICA Y SEGURIDAD EN MONTAÑA.............................................................. 50 l. Peligros en montaña 2. Vestuarioy equipo de montaña 3. Alimentación 4. Orientación Capítulo IV FISIOLOGÍA DE MONTAÑA ................................................................................ 69 1. Patología de la altitud 2. Aclimatización 3. Otraspatologías 4. Primeros auxilios 5. Aspectos psicológicos Capítulo V ACCIDENTES
    [Show full text]
  • Proceedingsof the 2Nd Palawan Research Symposium 2015 I
    Proceedingsof the 2nd Palawan Research Symposium 2015 i Science, Technology and Innovation for Sustainable Development nd Proceedings of the 2 Palawan Research Symposium 2015 National Research Forum on Palawan Sustainable Development 9-10 December 2015 Puerto Princesa City, Philippines Short extracts from this publication may be reproduced for individual use, even without permission, provided that this source is fully acknowledged. Reproduction for sale or other commercial purposes is however prohibited without the written consent of the publisher. Electronic copy is also available in www.pcsd.gov.ph and www.pkp.pcsd.gov.ph. Editorial Board: Director Josephine S. Matulac, Planning Director, PCSDS Engr. Madrono P.Cabrestante Jr, Knowledge Management Division Head, PCSDS Prof. Mildred P. Palon, Research Director, HTU Dr. Patrick A. Regoniel, Research Director, PSU Dr. Benjamin J. Gonzales, Vice President for Research, Development & Extension, WPU Exec. Dir. Nelson P. Devanadera, Executive Director, PCSDS Editorial Staff: Celso Quiling Bernard F. Mendoza Lyn S. Valdez Jenevieve P. Hara Published by: Palawan Council for Sustainable Development Staff-ECAN Knowledge Management PCSD Building, Sports Complex Road, Brgy. Sta. Monica,Puerto Princesa City Palawan, Philippines Tel. No. +63 48 434-4235, Telefax: +63 48 434-4234 www.pkp.pcsd.gov.ph Philippine Copyright ©2016 by PCSDS Palawan, Philippines ISBN: ___________ Suggested Citation: Matulac, J.L.S, M.P. Cabrestante, M.P. Palon, P.A. Regoniel, B.J. Gonzales, and N.P. Devanadera. Eds. 2016. Proceedings of the 2nd Palawan Research Symposium 2015. National Research Forum on Palawan Sustainable Development, “Science, Technology & Innovation. Puerto Princesa City, Palawan, Philippines. Proceedingsof the 2nd Palawan Research Symposium 2015 ii Acknowledgement The PCSDS and the symposium-workshop collaborators would like to acknowledge the following: For serving as secretariat, documenters, and facilitating the symposium, concurrent sessions and workshops: Prof.
    [Show full text]
  • Preliminary Catalog of the Sedimentary Basins of the United States
    Preliminary Catalog of the Sedimentary Basins of the United States By James L. Coleman, Jr., and Steven M. Cahan Open-File Report 2012–1111 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Coleman, J.L., Jr., and Cahan, S.M., 2012, Preliminary catalog of the sedimentary basins of the United States: U.S. Geological Survey Open-File Report 2012–1111, 27 p. (plus 4 figures and 1 table available as separate files) Available online at http://pubs.usgs.gov/of/2012/1111/. iii Contents Abstract ...........................................................................................................................................................1
    [Show full text]
  • And Gas-Based Geochemical Prospecting Of
    Water- and gas-based geochemical prospecting of geothermal reservoirs in the Tarapacà and Antofagasta regions of northern Chile Tassi, F.1, Aguilera, F.2, Vaselli, O.1,3, Medina, E.2, Tedesco, D.4,5, Delgado Huertas, A.6, Poreda, R.7 1) Department of Earth Sciences, University of Florence, Via G. La Pira 4, 50121, Florence, Italy 2) Departamento de Ciencias Geológicas, Universidad Católica del Norte, Av. Angamos 0610, 1280, Antofagasta, Chile 3) CNR-IGG Institute of Geosciences and Earth Resources, Via G. La Pira 4, 50121, Florence, Italy 4)Department of Environmental Sciences, 2nd University of Naples, Via Vivaldi 43, 81100 Caserta, Italy 5) CNR-IGAG National Research Council, Institute of Environmental Geology and Geo-Engineering, Pzz.e A. Moro, 00100 Roma, Italy. 6) CSIS Estacion Experimental de Zaidin, Prof. Albareda 1, 18008, Granada, Spain. 7) Department of Earth and Environmental Sciences, 227 Hutchinson Hall, Rochester, NY 14627, U.S.A.. Studied area The Andean Central Volcanic Zone, which runs parallel the Central Andean Cordillera crossing from North to This study is mainly focused on the geochemical characteristics of water and gas South the Tarapacà and Antofagasta regions of northern Chile, consists of several volcanoes that have shown phases of thermal fluids discharging in several geothermal areas of northern Chile historical and present activity (e.g. Tacora, Guallatiri, Isluga, Ollague, Putana, Lascar, Lastarria). Such an intense (Fig. 1); volcanism is produced by the subduction process thrusting the oceanic Nazca Plate beneath the South America Plate. The anomalous geothermal gradient related to the geodynamic assessment of this extended area gives El Tatio, Apacheta, Surire, Puchuldiza-Tuya also rise to intense geothermal activity not necessarily associated with the volcanic structures.
    [Show full text]
  • Reproductions Supplied by EDRS Are the Best That Can Be Made from the Ori Inal Document
    DOCUMENT RESUME ED 481 305 FL 027 837 AUTHOR Lo Bianco, Joseph, Ed. TITLE Voices from Phnom Penh. Development & Language: Global Influences & Local Effects. ISBN ISBN-1-876768-50-9 PUB DATE 2002-00-00 NOTE 362p. AVAILABLE FROM Language Australia Ltd., GPO Box 372F, Melbourne VIC 3001, Australia ($40). Web site: http://languageaustralia.com.au/. PUB TYPE Books (010) Collected Works Proceedings (021) EDRS PRICE EDRS Price MF01/PC15 Plus Postage. DESCRIPTORS *College School Cooperation; Community Development; Distance Education; Elementary Secondary Education; *English (Second Language); Ethnicity; Foreign Countries; Gender Issues; Higher Education; Indigenous Populations; Intercultural Communication; Language Usage; Language of Instruction; Literacy Education; Native Speakers; *Partnerships in Education; Preservice Teacher Education; Socioeconomic Status; Student Evaluation; Sustainable Development IDENTIFIERS Cambodia; China; East Timor; Language Policy; Laos; Malaysia; Open q^,-ity; Philippines; Self Monitoring; Sri Lanka; Sustainability; Vernacular Education; Vietnam ABSTRACT This collection of papers is based on the 5th International Conference on Language and Development: Defining the Role of Language in Development, held in Phnom Penh, Cambodia, in 2001. The 25 papers include the following: (1) "Destitution, Wealth, and Cultural Contest: Language and Development Connections" (Joseph Lo Bianco); (2) "English and East Timor" (Roslyn Appleby); (3) "Partnership in Initial Teacher Education" (Bao Kham and Phan Thi Bich Ngoc); (4) "Indigenous
    [Show full text]
  • Field Excursion Report 2010
    Presented at “Short Course on Geothermal Drilling, Resource Development and Power Plants”, organized by UNU-GTP and LaGeo, in Santa Tecla, El Salvador, January 16-22, 2011. GEOTHERMAL TRAINING PROGRAMME LaGeo S.A. de C.V. GEOTHERMAL ACTIVITY AND DEVELOPMENT IN SOUTH AMERICA: SHORT OVERVIEW OF THE STATUS IN BOLIVIA, CHILE, ECUADOR AND PERU Ingimar G. Haraldsson United Nations University Geothermal Training Programme Orkustofnun, Grensasvegi 9, 108 Reykjavik ICELAND [email protected] ABSTRACT South America holds vast stores of geothermal energy that are largely unexploited. These resources are largely the product of the convergence of the South American tectonic plate and the Nazca plate that has given rise to the Andes mountain chain, with its countless volcanoes. High-temperature geothermal resources in Bolivia, Chile, Ecuador and Peru are mainly associated with the volcanically active regions, although low temperature resources are also found outside them. All of these countries have a history of geothermal exploration, which has been reinvigorated with recent changes in global energy prices and the increased emphasis on renewables to combat global warming. The paper gives an overview of their main regions of geothermal activity and the latest developments in the geothermal sector are reviewed. 1. INTRODUCTION South America has abundant geothermal energy resources. In 1999, the Geothermal Energy Association estimated the continent’s potential for electricity generation from geothermal resources to be in the range of 3,970-8,610 MW, based on available information and assuming the use of technology available at that time (Gawell et al., 1999). Subsequent studies have put the potential much higher, as a preliminary analysis of Chile alone assumes a generation potential of 16,000 MW for at least 50 years from geothermal fluids with temperatures exceeding 150°C, extracted from within a depth of 3,000 m (Lahsen et al., 2010).
    [Show full text]
  • Recent Deformation Around Domuyo Volcano, Argentina Inferred from Time-Series Analyses of Insar Image
    SVC45-22 JpGU-AGU Joint Meeting 2020 Recent Deformation around Domuyo Volcano, Argentina Inferred from Time-series Analyses of InSAR Image *Satoshi Miura1, Micaela Colavita1, Yu Morishita2 1. Graduate School of Science, Tohoku University, 2. Geospatial Information Authority of Japan Domuyo volcano, located in the southern Central Andes of Argentina (36°37’S-70°26’W), is a Plio-Pleistocene dome complex hosting at least 14 dacitic lava domes (https://volcano.si.edu/ volcano.cfm?vn=357067) and other monogenetic basaltic centers (Astort et al., 2019). It occupies a retroarc position and can be found in the northernmost region of Cordillera del Viento (36°35’ to 36° 45’S), a N-S trending basement block crossed and rise by the Cortaderas lineament which is believed to exert a major structural control for the Neogene-to-Quaternary tectonic processes of the area (Galleto et al., 2018). With a height of 4,702 m the volcano constitutes the highest mountain in the Argentinian Patagonia and is related to an intense geothermal activity field that has been described as a fault controlled system associate with graben-like structures and shoshonitic volcanism developed under extensional regime during the Quaternary (Galleto et al., 2018). Without any historical eruption recorded this volcano was considered dormant, but the recent geophysical analysis has demonstrated unrest ongoing at the volcano. According to Astort et al. (2019), it has been growing at a rate of 12 cm/yr, calculated from the InSAR data. Along with seismic, gravimetric and morphometric data, they studied the deformation around the volcano using Sentinel-1 InSAR images from both ascending and descending orbits, within the 2014-2018 period of time.
    [Show full text]
  • Basement Composition and Basin Geometry Controls on Upper-Crustal Deformation in the Southern Central Andes (30–36° S)
    Geol. Mag.: page 1 of 17 c Cambridge University Press 2016 1 doi:10.1017/S0016756816000364 Basement composition and basin geometry controls on upper-crustal deformation in the Southern Central Andes (30–36° S) ∗ ∗ ∗ JOSÉ F. MESCUA †, LAURA GIAMBIAGI , MATÍAS BARRIONUEVO , ∗ ∗ ANDRÉS TASSARA‡, DIEGO MARDONEZ , MANUELA MAZZITELLI ∗ & ANA LOSSADA ∗ Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), Centro Científico Tecnológico Mendoza, CONICET. Av. Ruiz leal s/n Parque General San Martín, Mendoza (5500) Argentina ‡Departamento de Ciencias de la Tierra, Universidad de Concepción, Victor Lamas 1290, Barrio Universitario, Concepción, Casilla 160-C, Chile (Received 13 December 2015; accepted 5 April 2016) Abstract – Deformation and uplift in the Andes are a result of the subduction of the Nazca plate below South America. The deformation shows variations in structural style and shortening along and across the strike of the orogen, as a result of the dynamics of the subduction system and the features of the upper plate. In this work, we analyse the development of thin-skinned and thick-skinned fold and thrust belts in the Southern Central Andes (30–36° S). The pre-Andean history of the area determined the formation of different basement domains with distinct lithological compositions, as a result of terrane accretions during Palaeozoic time, the development of a widespread Permo-Triassic magmatic province and long-lasting arc activity. Basin development during Palaeozoic and Mesozoic times produced thick sedimentary successions in different parts of the study area. Based on estimations of strength for the different basement and sedimentary rocks, calculated using geophysical estimates of rock physical properties, we propose that the contrast in strength between basement and cover is the main control on structural style (thin- v.
    [Show full text]
  • The Political, Security, and Climate Landscape in Oceania
    The Political, Security, and Climate Landscape in Oceania Prepared for the US Department of Defense’s Center for Excellence in Disaster Management and Humanitarian Assistance May 2020 Written by: Jonah Bhide Grace Frazor Charlotte Gorman Claire Huitt Christopher Zimmer Under the supervision of Dr. Joshua Busby 2 Table of Contents Executive Summary 3 United States 8 Oceania 22 China 30 Australia 41 New Zealand 48 France 53 Japan 61 Policy Recommendations for US Government 66 3 Executive Summary Research Question The current strategic landscape in Oceania comprises a variety of complex and cross-cutting themes. The most salient of which is climate change and its impact on multilateral political networks, the security and resilience of governments, sustainable development, and geopolitical competition. These challenges pose both opportunities and threats to each regionally-invested government, including the United States — a power present in the region since the Second World War. This report sets out to answer the following questions: what are the current state of international affairs, complexities, risks, and potential opportunities regarding climate security ​ issues and geostrategic competition in Oceania? And, what policy recommendations and approaches should the US government explore to improve its regional standing and secure its national interests? The report serves as a primer to explain and analyze the region’s state of affairs, and to discuss possible ways forward for the US government. Given that we conducted research from August 2019 through May 2020, the global health crisis caused by the novel coronavirus added additional challenges like cancelling fieldwork travel. However, the pandemic has factored into some of the analysis in this report to offer a first look at what new opportunities and perils the United States will face in this space.
    [Show full text]
  • Modeling Subsurface Flow in Sedimentary Basins by CRAIG M
    129 Geologische Rundschau 78/1 I 129-154 I Stuttgart 1989 Modeling subsurface flow in sedimentary basins By CRAIG M. BETHKE, Urbana*) With 16 figures Zusammenfassung raines qui se manifestent dans les bassins sedimentaires, et qui resultent du relief topographique, de la convection, de la Grundwasserbewegungen in sedimentaren Becken, die compaction des sediments, de la decharge due l'erosio? et von dem topographischen Relief, konvektionsbedingtem a de la combinaison de ces divers facteurs. Dans ces modeles, Auftrieb, Sedimentkompaktion, isostatischen Ausgleichsbe­ on peut prendre en con~ideration les effets d~s tr:'nsferts d,e wegungen in Folge von Erosion und v~n ~mbinati~n~n chaleur et de matieres dlssoutes lors de la migration du pe­ dieser Kriifte gesteuert werden, konnen mit Hilfe quanutattv trole et ceux de I'interaction chimique de I'eau avec les modellierender Techniken beschrieben werden. In diesen roches. Toutefois la precision des previsions que I'on peut en Modellen kann man die Auswirkungen des Transports von deduire est limitee par la difficulte d'estimer I'echelle regia­ Warme und gel osten Stoffen, Petroleum-Migration und die a nale les proprietes hydrologiques des sediments, de reconsti­ chemische Interaktion zwischen Wasser und dem grund­ tuer les conditions anciennes, et de connaitre de quelle wasserleitenden Gestein beriicksichtigen. maniere les processus physiques et chimiques interferent Die Genauigkeit der Modell-Voraussagen ist allerdings a I'echelle des temps geologiques. La modelisation des bassins begrenzt wegen der Schwierigkeit, hydrologische Ei­ progressera dans la mesure ou la recherche hydrogeologique genschaften von Sedimenten in einem regionalen Rahmen ser mieux integree acelles d'autres disciplines telles que la se­ vorauszusagen, dem Schatzen vergangener Bedingungen und dimentologie, la mecanique des roches et la geochimie.
    [Show full text]
  • Yntfletic Fne]R OIL SHALE 0 COAL 0 OIL SANDS 0 NATURAL GAS
    2SO yntfletic fne]R OIL SHALE 0 COAL 0 OIL SANDS 0 NATURAL GAS VOLUME 28 - NUMBER 4- DECEMBER 1991 QUARTERLY Tsit Ertl Repository Artur Lakes Library C3orzdo School of M.ss © THE PACE CONSULTANTS INC. ® Reg . U.S. P.I. OFF. Pace Synthetic Fuels Report is published by The Pace Consultants Inc., as a multi-client service and is intended for the sole use of the clients or organizations affiliated with clients by virtue of a relationship equivalent to 51 percent or greater ownership. Pace Synthetic Fuels Report Is protected by the copyright laws of the United States; reproduction of any part of the publication requires the express permission of The Pace Con- sultants Inc. The Pace Consultants Inc., has provided energy consulting and engineering services since 1955. The company experience includes resource evalua- tion, process development and design, systems planning, marketing studies, licensor comparisons, environmental planning, and economic analysis. The Synthetic Fuels Analysis group prepares a variety of periodic and other reports analyzing developments In the energy field. THE PACE CONSULTANTS INC. SYNTHETIC FUELS ANALYSIS MANAGING EDITOR Jerry E. Sinor Pt Office Box 649 Niwot, Colorado 80544 (303) 652-2632 BUSINESS MANAGER Ronald L. Gist Post Office Box 53473 Houston, Texas 77052 (713) 669-8800 Telex: 77-4350 CONTENTS HIGHLIGHTS A-i I. GENERAL CORPORATIONS CSIRO Continues Strong Liquid Fuels Program 1-1 GOVERNMENT DOE Fossil Energy Budget Holds Its Ground 1-3 New SBIR Solicitation Covers Alternative Fuels 1-3 USA/USSR Workshop on Fossil Energy Held 1-8 ENERGY POLICY AND FORECASTS Politics More Important than Economics in Projecting Oil Market 1-10 Study by Environmental Groups Suggests Energy Use Could be Cut in Half 1-10 OTA Reports on U.S.
    [Show full text]
  • Krisenergy Ltd
    NOT FOR DISTRIBUTION, DIRECTLY OR INDIRECTLY, IN OR INTO THE UNITED STATES OR TO U.S. PERSONS CIRCULAR DATED 12 DECEMBER 2016 THIS CIRCULAR IS IMPORTANT AND REQUIRES YOUR IMMEDIATE ATTENTION. If you are in any doubt as to the action that you should take, you should consult your stockbroker, bank manager, solicitor, accountant or other professional adviser immediately. If you have sold or transferred all your shares in the capital of KrisEnergy Ltd. (the “Company”) of par value US$0.00125 each (“Shares”), please forward this Circular together with the Notice of Extraordinary General Meeting and the enclosed Depositor Proxy Form or Shareholder Proxy Form (as the case may be) immediately to the purchaser or transferee or to the agent through whom the sale or transfer was effected for onward transmission to the purchaser or transferee, subject to the distribution restrictions set out in this Circular. Approval in-principle has been obtained from the Singapore Exchange Securities Trading Limited (the “SGX-ST”) for the listing and quotation of the Notes, the Warrants and the New Shares (each as defined herein) on the Main Board of the SGX-ST, subject to certain conditions. The Notes, the Warrants and the New Shares will be admitted to the Main Board of the SGX-ST and official quotation will commence after all conditions imposed by the SGX-ST are satisfied, including (in the case of Warrants) there being a satisfactory spread of holdings of the Warrants to provide for an orderly market in the Warrants. The SGX-ST assumes no responsibility for the correctness or accuracy of any of the statements made, reports contained and opinions expressed in this Circular.
    [Show full text]