4: Potential Mineral Resources in Antarctica
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Sticta Arctica Degel.] Arctic Moon Habitat/Range: Over Mosses and Mossy Rocks in Alpine Localities; N Am – Eastern Eurasia, N to AK, S to OR
STICTA/UMBILICARIA [Sticta arctica Degel.] Arctic moon Habitat/Range: Over mosses and mossy rocks in alpine localities; N Am – eastern Eurasia, N to AK, S to OR. Reaction: All spot tests negative. Contents: No lichen substances reported. Notes: Not recorded from B.C., but known to occur in southern coastal Alaska only a few kilometres from the B.C. border. Sticta fuliginosa (Hoffm.) Ach. Peppered moon (sooty leather lichen) Habitat/Range: Frequent over deciduous trees and conifers, also over mossy rock, in humid forests at lower eleva- tions throughout, except absent from boreal regions; incompletely circumpolar, N to AK, S to CA. Reaction: All spot tests negative. Contents: No lichen substances reported. Sticta limbata (Sm.) Ach. Powdered moon Habitat/Range: Infrequent over deciduous trees and especially mossy rock in open coastal forests at lower eleva- tions, also rare in intermontane (ICH zone); western N Am – eastern N Am – western Eurasia, N to AK, S to CA. Reactions: All spot tests negative. Contents: No lichen substances reported. Sticta weigelii (Ach.) Vainio Map 107 Fringed moon (Weigel’s leather lichen) Habitat/Range: Rare over trees and shrubs in open coastal forests at lower elevations; western N Am – eastern N Am – eastern Eurasia, N to AK, S to CA. Reactions: All spot tests negative. Contents: No lichen substances reported. Sticta wrightii Tuck. Map 108 Green moon Habitat/Range: Rare over conifers in semi-shady intermontane old-growth forests at lower elevations; western N Am – eastern Eurasia, N to AK, S to BC. Reactions: All spot tests negative. Contents: No lichen substances reported. Sticta sp. -
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R. J. PANKHURST (CHIEF EDITOR) P. DOYLE E J. GREGORY J. S. GRIFFITHS A. J. HARTLEY R. E. HOLDSWORTH A. C. MORTON N. S. ROBINS M. S. STOKER J. P. TURNER Special Publication reviewing procedures The Society makes every effort to ensure that the scientific and production quality of its books matches that of its journals. Since 1997, all book proposals have been refereed by specialist reviewers as well as by the Society's Books Editorial Committee. If the referees identify weaknesses in the proposal, these must be addressed before the proposal is accepted. Once the book is accepted, the Society has a team of Book Editors (listed above) who ensure that the volume editors follow strict guidelines on refereeing and quality control. We insist that individual papers can only be accepted after satis- factory review by two independent referees. The questions on the review forms are similar to those for Journal of the Geological Society. The referees' forms and comments must be available to the Society's Book Editors on request. Although many of the books result from meetings, the editors are expected to commission papers that were not pre- sented at the meeting to ensure that the book provides a balanced coverage of the subject. Being accepted for presentation at the meeting does not guarantee inclusion in the book. Geological Society Special Publications are included in the ISI Science Citation Index, but they do not have an impact factor, the latter being applicable only to journals. -
The Undiscovered Oil and Gas of Antarctica
DEPARTMENT OF THE INTERIOR U.S. Geological Survey The Undiscovered Oil and Gas of Antarctica by John Kingston^ OPEN-FILE REPORT 91-597 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. ^Santa Barbara, California CONTENTS Page Abstract ....................................................... 1 Introduction ................................................... 2 Size of area .............................................. 2 Premise and problems of petroleum recoverability .......... 2 Previous investigations and petroleum assessments ......... 2 Methods of assessment ..................................... 4 Regional geology and petroleum occurrence ...................... 6 Assessment by play analysis .................................... 13 Rifted continental margin provinces ....................... 13 General; the south Australia rifted margin analog .... 13 Antarctica-Australia rift province ................... 17 Antarctica-India rift province ....................... 20 Antarctica-Africa rift province ...................... 24 Antarctica-Falkland rift province .................... 24 Interior rift provinces ................................... 30 General .............................................. 30 Ross sea interior rift province ...................... 30 Weddell sea interior rift province .................. -
Back Matter (PDF)
Index Page numbers in italic refer to tables, and those in bold to figures. accretionary orogens, defined 23 Namaqua-Natal Orogen 435-8 Africa, East SW Angola and NW Botswana 442 Congo-Sat Francisco Craton 4, 5, 35, 45-6, 49, 64 Umkondo Igneous Province 438-9 palaeomagnetic poles at 1100-700 Ma 37 Pan-African orogenic belts (650-450 Ma) 442-50 East African(-Antarctic) Orogen Damara-Lufilian Arc-Zambezi Belt 3, 435, accretion and deformation, Arabian-Nubian Shield 442-50 (ANS) 327-61 Katangan basaltic rocks 443,446 continuation of East Antarctic Orogen 263 Mwembeshi Shear Zone 442 E/W Gondwana suture 263-5 Neoproterozoic basin evolution and seafloor evolution 357-8 spreading 445-6 extensional collapse in DML 271-87 orogenesis 446-51 deformations 283-5 Ubendian and Kibaran Belts 445 Heimefront Shear Zone, DML 208,251, 252-3, within-plate magmatism and basin initiation 443-5 284, 415,417 Zambezi Belt 27,415 structural section, Neoproterozoic deformation, Zambezi Orogen 3, 5 Madagascar 365-72 Zambezi-Damara Belt 65, 67, 442-50 see also Arabian-Nubian Shield (ANS); Zimbabwe Belt, ophiolites 27 Mozambique Belt Zimbabwe Craton 427,433 Mozambique Belt evolution 60-1,291, 401-25 Zimbabwe-Kapvaal-Grunehogna Craton 42, 208, 250, carbonates 405.6 272-3 Dronning Mand Land 62-3 see also Pan-African eclogites and ophiolites 406-7 Africa, West 40-1 isotopic data Amazonia-Rio de la Plata megacraton 2-3, 40-1 crystallization and metamorphic ages 407-11 Birimian Orogen 24 Sm-Nd (T DM) 411-14 A1-Jifn Basin see Najd Fault System lithologies 402-7 Albany-Fraser-Wilkes -
Paleomagnetic and Geochronological Studies of the Mafic Dyke Swarms Of
Precambrian Research 198–199 (2012) 51–76 Contents lists available at SciVerse ScienceDirect Precambrian Research journa l homepage: www.elsevier.com/locate/precamres Paleomagnetic and geochronological studies of the mafic dyke swarms of Bundelkhand craton, central India: Implications for the tectonic evolution and paleogeographic reconstructions a,∗ a b a c Vimal R. Pradhan , Joseph G. Meert , Manoj K. Pandit , George Kamenov , Md. Erfan Ali Mondal a Department of Geological Sciences, University of Florida, 241 Williamson Hall, Gainesville, FL 32611, USA b Department of Geology, University of Rajasthan, Jaipur 302004, Rajasthan, India c Department of Geology, Aligarh Muslim University, Aligarh 202002, India a r t i c l e i n f o a b s t r a c t Article history: The paleogeographic position of India within the Paleoproterozoic Columbia and Mesoproterozoic Received 12 July 2011 Rodinia supercontinents is shrouded in uncertainty due to the paucity of high quality paleomagnetic Received in revised form 6 November 2011 data with strong age control. New paleomagnetic and geochronological data from the Precambrian mafic Accepted 18 November 2011 dykes intruding granitoids and supracrustals of the Archean Bundelkhand craton (BC) in northern Penin- Available online 28 November 2011 sular India is significant in constraining the position of India at 2.0 and 1.1 Ga. The dykes are ubiquitous within the craton and have variable orientations (NW–SE, NE–SW, ENE–WSW and E–W). Three dis- Keywords: tinct episodes of dyke intrusion are inferred from the paleomagnetic analysis of these dykes. The older Bundelkhand craton, Mafic dykes, Central ◦ NW–SE trending dykes yield a mean paleomagnetic direction with a declination = 155.3 and an incli- India, Paleomagnetism, Geochronology, ◦ ◦ − Ä ˛ Paleogeography nation = 7.8 ( = 21; 95 = 9.6 ). -
Biometric Comparisons Between North American and European Mammals
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Faculty Publications from the Harold W. Manter Laboratory of Parasitology Parasitology, Harold W. Manter Laboratory of 1959 Biometric Comparisons between North American and European Mammals. I. A Comparison between Alaskan and Fennoscandian Wolverine (Gulo gulo Linnaeus) Björn Kurtén Institute of Geology and Paleontology of Helsingfors University Robert L. Rausch Arctic Health Research Center, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/parasitologyfacpubs Part of the Parasitology Commons Kurtén, Björn and Rausch, Robert L., "Biometric Comparisons between North American and European Mammals. I. A Comparison between Alaskan and Fennoscandian Wolverine (Gulo gulo Linnaeus)" (1959). Faculty Publications from the Harold W. Manter Laboratory of Parasitology. 532. https://digitalcommons.unl.edu/parasitologyfacpubs/532 This Article is brought to you for free and open access by the Parasitology, Harold W. Manter Laboratory of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Faculty Publications from the Harold W. Manter Laboratory of Parasitology by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Björn Kurtén & Robert L. Rausch in Acta Arctica (1959) Fasc. XI. BIOMETRIC COMPARISONS BETWEEN NORTH AMERICAN AND EUROPEAN MAMMALS 1. A COMPARISON BETWEEN ALASK.AN AND FENNOSCANDIAN WOLVERINE (GULO GULO LINNAEUS) INTRODUCTION The taxonomy ofmany circumpolar mammals is not at present in a satis(;lctory state. Whercas many European students favour the circumpolar species concept, the approach or Amnican students has often had a provincial tinge. This attitude has been criticized by one ofus (IC\t:SCII, '953)· This holds also for the wolverine or glutton, subject ofthe present study: DEGER""!. -
Pan-African Orogeny 1
Encyclopedia 0f Geology (2004), vol. 1, Elsevier, Amsterdam AFRICA/Pan-African Orogeny 1 Contents Pan-African Orogeny North African Phanerozoic Rift Valley Within the Pan-African domains, two broad types of Pan-African Orogeny orogenic or mobile belts can be distinguished. One type consists predominantly of Neoproterozoic supracrustal and magmatic assemblages, many of juvenile (mantle- A Kröner, Universität Mainz, Mainz, Germany R J Stern, University of Texas-Dallas, Richardson derived) origin, with structural and metamorphic his- TX, USA tories that are similar to those in Phanerozoic collision and accretion belts. These belts expose upper to middle O 2005, Elsevier Ltd. All Rights Reserved. crustal levels and contain diagnostic features such as ophiolites, subduction- or collision-related granitoids, lntroduction island-arc or passive continental margin assemblages as well as exotic terranes that permit reconstruction of The term 'Pan-African' was coined by WQ Kennedy in their evolution in Phanerozoic-style plate tectonic scen- 1964 on the basis of an assessment of available Rb-Sr arios. Such belts include the Arabian-Nubian shield of and K-Ar ages in Africa. The Pan-African was inter- Arabia and north-east Africa (Figure 2), the Damara- preted as a tectono-thermal event, some 500 Ma ago, Kaoko-Gariep Belt and Lufilian Arc of south-central during which a number of mobile belts formed, sur- and south-western Africa, the West Congo Belt of rounding older cratons. The concept was then extended Angola and Congo Republic, the Trans-Sahara Belt of to the Gondwana continents (Figure 1) although West Africa, and the Rokelide and Mauretanian belts regional names were proposed such as Brasiliano along the western Part of the West African Craton for South America, Adelaidean for Australia, and (Figure 1). -
European Red List of Birds
European Red List of Birds Compiled by BirdLife International Published by the European Commission. opinion whatsoever on the part of the European Commission or BirdLife International concerning the legal status of any country, Citation: Publications of the European Communities. Design and layout by: Imre Sebestyén jr. / UNITgraphics.com Printed by: Pannónia Nyomda Picture credits on cover page: Fratercula arctica to continue into the future. © Ondrej Pelánek All photographs used in this publication remain the property of the original copyright holder (see individual captions for details). Photographs should not be reproduced or used in other contexts without written permission from the copyright holder. Available from: to your questions about the European Union Freephone number (*): 00 800 6 7 8 9 10 11 (*) Certain mobile telephone operators do not allow access to 00 800 numbers or these calls may be billed Published by the European Commission. A great deal of additional information on the European Union is available on the Internet. It can be accessed through the Europa server (http://europa.eu). Cataloguing data can be found at the end of this publication. ISBN: 978-92-79-47450-7 DOI: 10.2779/975810 © European Union, 2015 Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the source is fully acknowledged. Reproduction of this publication for resale or other commercial purposes is prohibited without prior written permission of the copyright holder. Printed in Hungary. European Red List of Birds Consortium iii Table of contents Acknowledgements ...................................................................................................................................................1 Executive summary ...................................................................................................................................................5 1. -
Terminal Suturing of Gondwana Along the Southern Margin of South China Craton: Evidence from Detrital Zircon U-Pb Ages and Hf Is
PUBLICATIONS Tectonics RESEARCH ARTICLE Terminal suturing of Gondwana along the southern 10.1002/2014TC003748 margin of South China Craton: Evidence from detrital Key Points: zircon U-Pb ages and Hf isotopes in Cambrian • Sanya of Hainan Island, China was linked with Western Australia in and Ordovician strata, Hainan Island the Cambrian • Sanya had not juxtaposed with South Yajun Xu1,2,3, Peter A. Cawood3,4, Yuansheng Du1,2, Zengqiu Zhong2, and Nigel C. Hughes5 China until the Ordovician • Gondwana terminally suture along the 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of southern margin of South China Geosciences, Wuhan, China, 2State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences, Wuhan, China, 3Department of Earth Sciences, University of St. Andrews, St. Andrews, UK, Supporting Information: 4Centre for Exploration Targeting, School of Earth and Environment, University of Western Australia, Crawley, Western • Readme Australia, Australia, 5Department of Earth Sciences, University of California, Riverside, California, USA • Figure S1 • Figure S2 • Table S1 • Table S2 Abstract Hainan Island, located near the southern end of mainland South China, consists of the Qiongzhong Block to the north and the Sanya Block to the south. In the Cambrian, these blocks were Correspondence to: separated by an intervening ocean. U-Pb ages and Hf isotope compositions of detrital zircons from the Y. Du, Cambrian succession in the Sanya Block suggest that the unit contains detritus derived from late [email protected] Paleoproterozoic and Mesoproterozoic units along the western margin of the West Australia Craton (e.g., Northampton Complex) or the Albany-Fraser-Wilkes orogen, which separates the West Australia and Citation: Mawson cratons. -
Geological Studies in Western Muhlig-Hofmann Mountains, Central Dronning Maud Land, East Antarctica
Twenty Second Indian Expedition to Antarctica, Scientific Report, 2008 Ministry of Earth Sciences, Technical Publication No. 20, pp 177-189 Geological Studies in Western Muhlig-Hofmann Mountains, Central Dronning Maud Land, East Antarctica A. Dharwaclkar, R. Asthana, K. Kachroo, L.K. Oberoi and Aran Chaturvedi Geological Survey of India INTRODUCTION In pursuance of its long term program of mapping the entire Wohlthat ranges in cDML, East Antarctica, geological mapping was carried out in the western parts of Muhlig-Hofmann Mountains during the 22nd Indian Antarctic Expedition. About 1000 sq km area bounded by Longitudes 5°00' and 5°45' East and Latitudes 71°45' and 72° 10' South was covered during the austral summer of 2002-03. The study area lies more than 170NM WSW of Maitri station and the fieldwork was carried out using helicopters by taking drop- points in the area. GEOLOGICAL SETTING The East Antarctic shield is mostly composed of Precambrian crystalline rocks and has undergone a complex tectono-metamorphic history (Ravich & Kamenev, 1975; Sengupta, 1988; Tingey, 1991; D'Souza et al., 1997). The cDML basically consists of polymetamorphosed metasedimentary rocks represented by garnet-biotite schists, hornblende gneisses, metapelites, calc- silicates etc. These are intruded by various inagmatic units like anorthosite, granodiorite, granite, monzonite, charnockite and other minor instrusives. The deformational record of the region indicates a granulite facies metamorphism (Grenvillian) superimposed by later Pan-African (amphibolite to granulite) event. Record of the earlier Grenvillian event is preserved in the pelitic/ semipelitic schists and mafic granulites. (Jacobs et al., 2003). The Muhlig-Hofmann Mountains occurring in the western part of cDML are dominated by magmatic phase with large plutons of charnockite, granite and syenite forming the intrusive phase. -
Weather Satellite Views Iceberg
National Weather Digest WEATHER SATELLITE VIEWS ICEBERG by Henry W. Brandli (1) During the first week in November 1987, an iceberg, twice to the shore of the Arabian Peninsula. Officials say that the size of the state of Rhode Island, broke away from Ant satellites will be used to spot the masses of ice that tugboats arctica and was drifting in the Ross Sea. The iceberg broke will move toward the equator. Researchers estimate the proj from the Ross Ice Shelf, a region of freshwater ice formed ect will take several months. The icebergs' massiveness should from snow, at a point called the Bay of Whales. keep them from melting away in transit." Icebergs often break away from the Antarctic ice shelves Earth resources satellites of the US, France and Russia, where they are affected by weather and tidal forces. This also can view the iceberg, but not as frequently as polar new iceberg (B 9) equaled two to three times the amount of orbiting weather spacecraft. Also, weather satellite imagery ice that normally breaks free in a year. On 19 February 1988 , (visual/infrared, microwave, etc.) provide other important the Defense Meteorological Satellite (DMSP) obtained a visual factors affecting the giant "ice cube," i.e. wind , water tem view of the iceberg (Fig. I). The iceberg was about 25 miles peratures, ocean currents, rain, etc. And the DMSP has the wide and 98 miles long, for an area of2,450 square miles and best resolution of any meteorological satellite. estimated at 750 feet thick. An interesting concept appeared in a recent issue ofInsight Magazine: "Equatorial lands in need offresh water may soon NOTES AND REFERENCES have access to a new source, Antarctic icebergs. -
Geology of Antarctica
GEOLOGY OF ANTARCTICA 1. Global context of Antarctica Compared with other continents, the geological evolution of Antarctica is relatively little known, since less than 2% of the land emerges from beneath the thick cover of glacier ice. Yet where rocks are exposed, their pristine nature and lack of vegetation has enabled geologists to unravel many key components of the region’s history. In addition, the use of geophysical and remote sensing techniques, together with drilling on the Continental Shelf, has helped resolve many of the geological questions posed by the limited outcrop. Antarctica is the remotest of the world’s continents, with its nearest neighbour being South America, some 100 km (560 miles) distant. Yet, relatively early on in the geological exploration of Antarctica it was recognized that Antarctica shared a common history with other southern hemisphere continents, such as South America, Africa, Arabia, India and Australasia. However, these early ideas of movement of continents by joining together, followed by splitting apart, were ridiculed by many geologists and geophysicists, until the revolution in geological thinking in the late 1960s that led to the ‘theory of plate tectonics’. This collection of photographs is assembled to capture the spirit of Antarctica’s geological evolution, grouped according to the key events that have shaped the continent. A limited knowledge of geological processes and terms is required to fully appreciate this set. Conditions of use of images 1 Contributors (who retain copyright), to whom requests for reproduction should be sent, are listed after the caption by their initials. In general, reproduction of these relatively low-resolution images is permitted for educational purposes without prior permission, e.g.