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EPSC2013-476, 2013 European Planetary Science Congress 2013 Eeuropeapn Planetarsy Science Ccongress C Author(S) 2013
EPSC Abstracts Vol. 8, EPSC2013-476, 2013 European Planetary Science Congress 2013 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2013 Geology and astrobiological implications of Argyre, Mars J.M. Dohm (1), R. El-Maarry (2), R.J. Soare (3), J.-P. Williams (4), S.J. Conway (5), H. Miyamoto (6), and S. Maruyama (1) (1) Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo, Japan 152-8551 ([email protected]), (2) Physikalisches Institut, Bern Universität, Berne, Switzerland 3012, (3) Geography Department, Dawson College, Montreal, Canada H3Z 1A4, (4) Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, (5) Department of Physical Sciences, Open University, Milton Keynes, United Kingdom MK7 6AA, (6) The Museum, The University of Tokyo, Tokyo, Japan 113-003 1. Introduction investigation includes the Argyre floor and rim, transition zone, and the southeast margin of the Thaumasia plateau Using Viking and post-Viking data, the detailed [1]. Also shown is a newly identified paleolake basin (wide geological investigation of the Argyre impact basin arrow) located on the western margin of the Argyre impact and surroundings (30°S to 65°S, 290°E to 340.0°E; basin and the Uzboi drainage system (narrow arrows), Fig.1) has: (1) resulted in a new geologic map of the possible spillway separating the paleolake basin from the region (Fig.2); (2) revealed the stratigraphical history Argyre basin at a present-day topographic interval nearing of the region, including distinct sequence stratigraphy 1.5 km (dashed line), and a transect for topographic profile marking a lake that formed shortly after the Argyre shown in Fig. -
Geodiversity, Geoconservation and Geotourism in Hong Kong Global
Proceedings of the Geologists’ Association 126 (2015) 426–437 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola Geodiversity, geoconservation and geotourism in Hong Kong Global Geopark of China Lulin Wang *, Mingzhong Tian, Lei Wang School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China A R T I C L E I N F O A B S T R A C T Article history: In addition to being an international financial center, Hong Kong has rich geodiversity, in terms of a Received 22 November 2014 representative and comprehensive system of coastal landscapes, with scientific value in the study of Received in revised form 20 February 2015 Quaternary global sea-level changes, and esthetic, recreational and cultural value for tourism. The value Accepted 26 February 2015 of the coastal landscapes in Hong Kong was globally recognized when Hong Kong Global Geopark Available online 14 April 2015 (HKGG), which was developed under the well-established framework of Hong Kong Country Parks and Marine Parks, was accepted in the Global Geoparks Network (GGN) in 2011. With over 30 years of Keywords: experience gained from managing protected areas and a concerted effort to develop geoconservation and Coastal landscape geotourism, HKGG has reached a mature stage of development and can provide a well-developed Hong Kong Global Geopark Geodiversity example of successful geoconservation and geotourism in China. This paper analyzes the geodiversity, Geoconservation geoconservation and geotourism of HKGG. The main accomplishments summarized in this paper are Geotourism efficient conservation management, an optimized tourism infrastructure, a strong scientific interpretation system, mass promotion and education materials, active exchange with other geoparks, continuous training, and effective collaboration with local communities. -
Geological Society of Hong Kong Newsletter Vol.19, Issue No
Geological Society of Hong Kong Newsletter Vol.19, Issue No. 1 GEOLOGICAL SOCIETY OF HONG KONG NEWSLETTER Volume 19, Issue No. 1, March, 2013 Website: www.geolsoc.org.hk/newsletters.htm ; Editor: George Tsang “Contemporary Chinese Geoscientists” by of these kind of rocks; He used plate George Tsang tectonics to study the formation of “Large igneous province” and its relationship with This issue we continue the interviews for the metallogeny in eastern China in Mesozoic respective academicians, the articles are era. arranged in the alphabetical order of their family names. We have Professors WANG, De-zi and Professor XUE, Yu-qun from Nanjing University and Professor YIN, Hong-fu from China University of Geosciences (Wuhan). We thank the kind acceptance of the interviews and the review of the academicians for their articles. Professor Wang was born in 1927 in a teacher‟s family in Tai Xing County (泰興 縣), Jiang Su province. His father was a teacher. His mother passed away when he was 7 and his father followed when he was 9, he was brought up by his two sisters, the parents were survived by five children, Contemporary Geoscientists of China Professor Wang is the fourth. - WANG, De-zi (花崗岩專家王德滋院士) Professor Wang is a petrologist in the field of granite and volcanic rocks. He was the first in China to raise the concept of “subvolcanic granitoids” which concerns the intrusion of subvolcanic granitoids into complex rock considering from time, space and source of materials; He found the first S type volcanic rock in China and classified it into water rich, water deficient and fluorine rich associations, which provide new concept for the formation Interview at his residence 1 Professor Wang completed his lower high confirmed his decision to devote his life into school course under a very arduous condition geology. -
History of Mining in Hong Kong
23rd April 2015 Hong Kong Regional Group, Geological Society of London Jackie C.T. Chu SUPPORTED BY CONTENT • Minerals in Hong Kong • Mines Site in Hong Kong MINERALS IN HONG KONG • Galena • Beryl • Lin Ma Hang • Devil’s Peak • Mui Wo • Graphite • Lead Mine Pass • West Brother Island • Wolframite • Needle Hill • Quartz, Feldspar, Kaolin • Sheung Tong • Chek Lap Kok • Castle Peak • Cha Kwo Ling • Magnetite • Wun Yiu • Ma On Shan • Sha Lo Wan GALENA N 0 5 km LIN MA HANG (1860-1962) GALENA N 0 5 km MUI WO (1619-1896) GALENA N 0 5 km MAP OF SAN ON DISTRICT (1866) Courtesy of National Library of Australia NG TUNG CHAI (19TH CENTURY TO UNKNOWN) NG TUNG CHAI WOLFRAMITE N 0 5 km NEEDLE HILL (1917-1967) NEEDLE HILL (1917-1967) WOLFRAMITE N 0 5 km SHEUNG TONG (1951-1970) WOLFRAMITE N 0 5 km CASTLE PEAK (1952) CASTLE PEAK (1952) MAGNETITE N 0 5 km MA ON SHAN (1906-1981) Open Pit ( 1906- 1959) Underground ( 1953- 1981) MA ON SHAN (1906-1981) MA ON SHAN (1906-1981) BERYL N 0 5 km DEVIL’S PEAK (1957) DEVIL’S PEAK (1957) GRAPHITE N 0 5 km WEST BROTHER ISLAND (1952-1971) WEST BROTHER ISLAND (1952-1971) WEST BROTHER ISLAND (1952-1971) QUARTZ FELDSPAR KAOLIN N 0 5 km CHEK LAP KOK (1959-1988) Hong Kong International Airport Ngong Ping 360 Cable Car QUARTZ FELDSPAR KAOLIN N 0 5 km CHA KWO LING (1950S-1990S) AND …… QUARRIES N 0 5 km FOUR HILLS OF KOWLOON SEA DEFENCES MAP (1876) LEI YUE MUN LAM TEI MT. -
Coal Mine Methane Country Profiles, June 2015
Disclaimer The U.S. Environmental Protection Agency does not: a) Make any warranty or representation, expressed or implied, with respect to the accuracy, completeness, or usefulness of the information contained in this report, or that the use of any apparatus, method, or process disclosed in this report may not infringe upon privately owned rights; or b) Assume any liability with respect to the use of, or damages resulting from the use of, any information, apparatus, method, or process disclosed in this report. CMM Country Profiles CONTENTS Units of Conversions .............................................................................................................................................. i Executive Summary .............................................................................................................................................. ii Global Overview at a Glance ................................................................................................................................. ii Introduction ............................................................................................................................................................ 1 Purpose of the Report ............................................................................................................................................. 2 Organization of the Report ................................................................................................................................... 2 1 Argentina ...................................................................................................................................................... -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
Landslide Hazard Analysis for Hong Kong Using Landslide Inventory And
ARTICLE IN PRESS Computers & Geosciences 30 (2004) 429–443 Landslide hazard analysis for HongKongusing landslide inventory and GIS K.T. Chau*, Y.L. Sze, M.K. Fung, W.Y. Wong, E.L. Fong, L.C.P. Chan Department of Civil and Structural Engineering, The Hong Kong Polytechnic University, Yuk Choi Road, Hung Hom, Kowloon, Hong Kong, China Received 20 February 2002; accepted 5 August 2003 Abstract This paper presents a landslide-inventory-based and GIS-based framework for systematic landslide hazard analysis by employing historical landslide data in Hong Kong, coupling with geological, geomorphological, population, climatic, and rainfall data. Based on 1448 landslide data from 1984 to 1998, the diurnal and seasonal distributions of landslides are established and compared with the seasonal rainfall variation. The cumulative fatalities and injuries caused by landslides increase with the cumulative rainfall in HongKong,indicatinga strongcorrelation between rainfall and landslide consequences. The averageannual fatality and injury rates in HongKongcaused by landslide are 11.35 and 11.63, respectively. In terms of beinghit by a landslide, squatter areas and roads on HongKongIsland are at the highest risk. A frequency–volume relation for Hong Kong Island was established, and, using this relation, it was estimated that the return period of a 26,000 m3 landslide (the size of 1995 Shum Wan Road Landslide) is about 3.12 years. A hazard zonation map for HongKongIsland is established by usinghistorical data. The potential use of GIS technology to incorporate various layers of information is illustrated using Hong Kong Island as an example. Both landslide hazard and risk maps are proposed usingraster calculation. -
Alternative Model for the Derivation of Gold in the Witwatersrand Supergroup
J. geol. Soc. London, Vol. 141, 1984, pp. 263-272, 3 figs., 3 tables. Printed in Northern Ireland. Alternative model for the derivation of gold in the Witwatersrand Supergroup Thomas 0. Reimer SUMMARY: Present models of the derivation of the gold in the Witwatersrand conglomerates of South Africa as detrital grains directly from primary deposits in a source area consisting mainly of Archaean schist belts meets with a volume problem. Witwatersrand deposits have yielded about 923 kg/km2 Au compared to about 65 kg/km* Au in the richest known schist belts. Differences in the extent of mining activities cannot account for these differences in yield. Gold fineness, grain size, and morphology of the gold particles are also difficult to reconcile with a purely detrital derivation. Data on the mobility of gold in the hydrosphere and in the weatheringcycle are used to erect a model which predicts that mostof the gold in the Witwatersrand conglomerates was derived from a source area in trace amounts in a ‘dissolved’ form and precipitated at or close to the edge of the depositional basin, possibly under organic influences. Subsequent sedimentary reworking and metamorphiddiagenetic remobilization led to the formation of the complex association of minerals observed now in the conglomerates. Since the dawn of civilization an estimatedtotal of data irreconcilable with the ‘mechanical’ model of about 65 000 tons of gold has been produced. Of this derivation of the Witwatersrand gold. Atthe same about 55% has beenderived fromthe auriferous time an alternative model for the processes which led conglomerates of the early Proterozoic Witwatersrand tothe spectacularconcentration of gold in these Supergroup (2.3-2.7 Ga.). -
GEO REPORT No. 282
EXPERT REPORT ON THE GEOLOGY OF THE PROPOSED GEOPARK IN HONG KONG GEO REPORT No. 282 R.J. Sewell & D.L.K. Tang GEOTECHNICAL ENGINEERING OFFICE CIVIL ENGINEERING AND DEVELOPMENT DEPARTMENT THE GOVERNMENT OF THE HONG KONG SPECIAL ADMINISTRATIVE REGION EXPERT REPORT ON THE GEOLOGY OF THE PROPOSED GEOPARK IN HONG KONG GEO REPORT No. 282 R.J. Sewell & D.L.K. Tang This report was originally produced in June 2009 as GEO Geological Report No. GR 2/2009 2 © The Government of the Hong Kong Special Administrative Region First published, July 2013 Prepared by: Geotechnical Engineering Office, Civil Engineering and Development Department, Civil Engineering and Development Building, 101 Princess Margaret Road, Homantin, Kowloon, Hong Kong. - 3 - PREFACE In keeping with our policy of releasing information which may be of general interest to the geotechnical profession and the public, we make available selected internal reports in a series of publications termed the GEO Report series. The GEO Reports can be downloaded from the website of the Civil Engineering and Development Department (http://www.cedd.gov.hk) on the Internet. Printed copies are also available for some GEO Reports. For printed copies, a charge is made to cover the cost of printing. The Geotechnical Engineering Office also produces documents specifically for publication in print. These include guidance documents and results of comprehensive reviews. They can also be downloaded from the above website. The publications and the printed GEO Reports may be obtained from the Government’s Information Services Department. Information on how to purchase these documents is given on the second last page of this report. -
Slope Superficial Displacement Monitoring by Small Baseline SAR
Remote Sens. 2014, 6, 1564-1586; doi:10.3390/rs6021564 OPEN ACCESS remote sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Slope Superficial Displacement Monitoring by Small Baseline SAR Interferometry Using Data from L-band ALOS PALSAR and X-band TerraSAR: A Case Study of Hong Kong, China Fulong Chen 1,2,*, Hui Lin 3,4 and Xianzhi Hu 3 1 Key Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, No. 9 Dengzhuang South Road, Haidian District, Beijing 100094, China 2 International Centre on Space Technologies for Natural and Cultural Heritage under the Auspices of UNESCO, No. 9 Dengzhuang South Road, Haidian District, Beijing 100094, China 3 Institute of Space and Earth Information Science, The Chinese University of Hong Kong, ShaTin, Hong Kong 999077, China; E-Mails: [email protected] (H.L.); [email protected] (X.H.) 4 Department of Geography and Resource Management, The Chinese University of Hong Kong, ShaTin, Hong Kong 999077, China * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +86-10-8217-8198; Fax: +86-10-8217-8915. Received: 12 December 2013; in revised form: 27 January 2014 / Accepted: 10 February 2014 / Published: 20 February 2014 Abstract: Owing to the development of spaceborne synthetic aperture radar (SAR) platforms, and in particular the increase in the availability of multi-source (multi-band and multi-resolution) data, it is now feasible to design a surface displacement monitoring application using multi-temporal SAR interferometry (MT-InSAR). Landslides have high socio-economic impacts in many countries because of potential geo-hazards and heavy casualties. -
Maceral Types and Quality of Coal in the Tuli Coalfield: a Case
applied sciences Article Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of Coal in the Madzaringwe Formation in the Vele Colliery, Limpopo Province, South Africa Elelwani Denge * and Christopher Baiyegunhi Department of Geology and Mining, University of Limpopo, Private Bag X1106, Sovenga 0727, South Africa; [email protected] * Correspondence: [email protected] Featured Application: Authors are encouraged to provide a concise description of the specific application or a potential application of the work. This section is not mandatory. Abstract: The Madzaringwe Formation in the Vele colliery is one of the coal-bearing Late Palaeozoic units of the Karoo Supergroup, consisting of shale with thin coal seams and sandstones. Maceral group analysis was conducted on seven representative coal samples collected from three existing boreholes—OV125149, OV125156, and OV125160—in the Vele colliery to determine the coal rank and other intrinsic characteristics of the coal. The petrographic characterization revealed that vitrinite is the dominant maceral group in the coals, representing up to 81–92 vol.% (mmf) of the total sample. Collotellinite is the dominant vitrinite maceral, with a total count varying between 52.4 vol.% (mmf) and 74.9 vol.% (mmf), followed by corpogelinite, collodetrinite, tellinite, and pseudovitrinite with a Citation: Denge, E.; Baiyegunhi, C. count ranging between 0.8 and 19.4 vol.% (mmf), 1.5 and 17.5 vol.% (mmf), 0.8 and 6.5 vol.% (mmf) Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of and 0.3 and 5.9 vol.% (mmf), respectively. The dominance of collotellinite gives a clear indication Coal in the Madzaringwe Formation that the coals are derived from the parenchymatous and woody tissues of roots, stems, and leaves. -
National Accounts
National Accounts Environmental Economic Accounts Mineral Accounts for South Africa: 1990–2010 Discussion document: D0405.2 March 2013 your leading partner in quality statistics Please scroll down Mineral Accounts for South Africa: 1990–2010 Discussion document: D0405.2 March 2013 Statistics South Africa Published by Statistics South Africa, Private Bag X44, Pretoria 0001 © Statistics South Africa, 2013 Users may apply or process this data, provided Statistics South Africa (Stats SA) is acknowledged as the original source of the data; that it is specified that the application and/or analysis is the result of the user's independent processing of the data; and that neither the basic data nor any reprocessed version or application thereof may be sold or offered for sale in any form whatsoever without prior permission from Stats SA. Discussion document: Mineral Accounts for South Africa: 1990–2010 Discussion document (D0405.2) Statistics South Africa Pretoria: Statistics South Africa, March 2013 A complete set of Statistics South Africa publications is available at the Statistics South Africa Library and the following libraries: National Library of South Africa, Pretoria Division National Library of South Africa, Cape Town Division Library of Parliament, Cape Town Bloemfontein Public Library Natal Society Library, Pietermaritzburg Johannesburg Public Library Eastern Cape Library Services, King William's Town Central Regional Library, Polokwane Central Reference Library, Nelspruit Central Reference Collection, Kimberley Central Reference Library, Mmabatho This discussion document is available on the Statistics South Africa internet site: www.statssa.gov.za Statistics South Africa Table of contents Figures, maps and tables iii Abbreviations and acronyms v Key findings 1 1.