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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Primary terms
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metal ores
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lead ores (3)
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lead-zinc deposits (6)
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metals
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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schalenblende
The birefringence-structural state relation in natural zinc sulfides and its application to a schalenblende from Pribram
Photomicrographs (plane-polarised light) of the sulphide mineralisation. (A...
Mineralogy, paragenesis, and mineral zoning of the West Fork Mine, Virburnum Trend, Southeast Missouri
Microbial Sphalerite Formation in Carbonate-Hosted Zn-Pb Ores, Bleiberg, Austria: Micro- to Nanotextural and Sulfur Isotope Evidence
Elementary composition of sphalerite. (A–C) Chemical mapping (Cd and Fe) by...
F ig . 8. Photomicrographs showing textures in the sphalerite ores (transmi...
Distribution of trace elements in willemite from the Belgium non-sulphide deposits
AN ATYPICAL OREBODY IN THE BRUSHY CREEK MINE, VIBURNUM TREND, MVT DISTRICT, MISSOURI: EARLY Cu-(Ni-Co)-Zn-RICH ORES AT THE LAMOTTE SANDSTONE/BONNETERRE DOLOMITE CONTACT
A. to E. Transmitted PPL photomicrographs of sphalerite colors and textures...
(A) Photograph of hand specimen from the first Cardita horizon showing rhyt...
Geology and Geochemistry of the Reocín Zinc-Lead Deposit, Basque-Cantabrian Basin, Northern Spain
S 3 : SULFIDES, STRUCTURES AND SYNCHROTRON LIGHT A TRIBUTE TO MICHAEL E. FLEET: PREFACE
Carbonate-Hosted Zn-Pb Deposits in Upper Silesia, Poland: Origin and Evolution of Mineralizing Fluids and Constraints on Genetic Models
Thallium geochemistry in the metamorphic Lengenbach sulfide deposit, Switzerland: Thallium-isotope fractionation in a sulfide melt
Processes of Enrichment of Trace Metals for High-Tech Applications in Hydrothermal Veins of the Ruhr Basin and the Rhenish Massif, Germany
SEQUENCE OF DIAGENETIC AND MINERALIZATION EVENTS, PINE POINT LEAD-ZINC PROPERTY, NORTHWEST TERRITORIES, CANADA
Phase Equilibria at High Temperatures
Abstract Several of the mineral belts of Southeast Asia pass through Thailand and knowledge of the ore types and metalliferous potential of Thailand may be key to understanding the metallo-genesis of the Southeast Asia region. In 2004, the mining and quarrying sector of Thailand contributed 2.29% to the Gross Domestic Product (GDP) and in 2006 the most valuable minerals produced were coal, gold, gypsum, limestone and zinc ( Wu 2008 ). Minerals and their mineral products have played an important part in the development of the infrastructure and the economy of Thailand in recent years, coming third after agriculture and tourism. The statistics for the mining of metalliferous minerals and the quantities of some derived mineral products in Thailand between 2001 and 2007 are summarized in Table 17.1 . In several instances, rising local demand for a mineral product far exceeds domestic mine output (e.g., the production of steel from iron ore and of antimony) and the shortfall is made up by the import of scrap and mineral ores for processing in the smelter industry. On the other hand, tin mining was for many decades an important activity in Thailand but has declined in recent years in response to reduced international demand. The closure of the majority of the former tin mines has prevented the Thai mining sector benefiting from the recent rise in global metal demand and prices, although the well-established tin smelter industry continues in business and produces tin products for the domestic and overseas markets through the