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Genesis of gold and antimony deposits in the Youjiang metallogenic province SW China Evidence from in situ oxygen isotopic and trace element compositions of quartz 0 : 99 : JLA B RHA B JX A
·Exploration for Antimony Deposits in Southern Tuscany Italy R M Dehm D D Klemm C M[Jller J Wagner and K Weber Diefenbach which generally are expected to be the primary source of antimony From these pre Variscan units antimony was remobilized and transport ed hydrothermally to its present position 1 GEOLOGICAL SETTING AND
·Large Sb mines are located in the ZR Basin including the Longshan Sb Au mine Xikuangshan Sb mine Gutaishan Sb mine Zhazixi Sb mine and Banxi Sb mine from upstream to downstream Fig 1 and Table S1 The Longshan Sb Au mine is located in the Longshan Shaoshui catchment and the wastewater from this mine flows into the ZR between sampling
Stibnite is commonly found as one of the primary ore minerals in most antimony deposits and it can even occur as the sole ore mineral in some large antimony deposits; therefore sulfur isotope
The idealized prototype of a southern Tuscan antimony deposit can be described as follows The irregular mineralization is situated in the upper part of the highly porous Calcare Cavernoso overlain by an impermeable unit normally a flysch type rock The deposits are bound to the edge of horst positions and also to areas of elevated geothermal gradient and resulting
·The Kharma antimony deposit in the Cordillera Oriental Bolivia is representative of vein type antimony deposits that have stibnite as the only mineral of economic interest and a low gold content In this deposit recovery of gold is difficult because it is not known exactly where the gold is located within the ore shoots or the manner in which it is present in the main
PDF On Jan 1 2013 N P Shen and others published Characteristics of sulfur and lead isotopes for Banian antimony deposit in Dushan area Guizhou province China Implication for origin of ore
·China is one of the first countries in the world to discover and mine Sb deposits ≪Chinese mineral deposits≫ editorial committee 1989 Antimony reserves and production are abundant in China Niu et al 2012 which ranks first in the world and play a significant role in the global production and trade of Sb Zhou et al 2014
5 ·Located in western Slovakia it potentially hosts one of the European Union s most significant known primary antimony deposits 63 holes were historically completed into the deposit during the 1980 1900s over a strike length of kilometers along with nearly kilometers of underground workings; the deposit hosts historical non
Remarkably there is a distinct disparity in the distribution of Sn deposits across Thailand In the eastern regions dominated by granitic rocks Sn deposits are almost absent Fig 1 In sharp contrast the granitic formations along the Thai Myanmar border in western central Thailand host numerous economically substantial Sn ore deposits Hutchison and Taylor 1978 Lehmann et
The Sulfur and lead isotopic compositions of stibnite from Banian antimony deposit located in Dushan County Guizhou Province one of representative antimony deposits in the South China Sb belt whose orebodies hosted by the Dushan Formation of the Middle Devonian were systematically analyzed in this results show that δ34S values of stibnite range from
Classification and Distribution of Antimony Deposits in China Xiongwei Hu 1 Satoshi MURAO Mingkui SHI and Buo LI Abstract China ranks the first in the world both for antimony production and its reserves There are about 600 occurrences in China Based on the occurrence mode of ore five types are distinguished for the antimony deposits
·Antimony can be re covered as either a primary commodity from some deposits or as a by product commodity from some gold or silver deposits Environmental risks associated with antimony mining include those related to mining in general such as the acid generating potential of solid mine waste and some issues specific to antimony as described
·Antimony is classified as a critical/strategic metal Its primary production is predominated by China via pyrometallurgical routes such as volatilization roasting—reduction smelting or direct reduction smelting The performance of most of the pyro processes is very sensitive to concentrate type and grade Therefore technology selection for a greenfield plant
The quartz stibnite scheelite and quartz stibnite cinnabar associations are characteristic of the calcareous formations of Paleozoic age whereas the quartz antimony mercury assemblage occurs only in the lower Carboniferous of the Cantabrian Iberian antimony deposits are interpreted to be the result of direct or indirect magmatic
·Antimony has been produced from ores in over 15 countries As shown in Table 2 world reserves of antimony are estimated to about million metric tonnes and in 2016 global antimony
·Despite the Xiangzhong metallogenic province being globally the most important ore concentrated area of antimony Sb mineralization the genesis of Sb Au W deposits in this region is still
The tin deposits associated with biotite granite 184 230 Ma that made up Main Range Granitoid district in Peninsular Malaysia Belt 1 Tin belt southern Peninsular Thailand and Central Thailand contributed over 55% of the tin production of Southeast Asia Schwartz et al 1995
·Majority of antimony bearing ore deposits are associated with the subduction related western Pacific plate boundaries especially in east and south east Asia The highest antimony concentrations commonly occur in low temperature magmatic hydrothermal systems in the epithermal environment Gold quartz carbonate vein deposits occur in deformed
·Orogenic antimony gold deposits contribute significantly to the global antimony resource base China s orogenic antimony gold deposits are primarily in southern Tibet Investigations indicate that antimony combines and migrates with sulfur hydroxides in ore forming fluids Previous research on fluid inclusions in orogenic antimony gold ores with sedimentary
The Shalagang Sb deposit is located at 40km southeast of the Ranba complex dome at the Northern Himalaya area in China At least four mineralization styles are recognized in Northern Himalaya 1 Au deposits; 2 Sb Au deposits; 3 Sb deposits and 4 Pb Zn Ag Sb deposits Shalagang is one of representative vein type antimony deposits that have stibnite as the only
Banpo antimony deposit is a typical fracture controlling and hydrothermal fluid filling deposit Geochemical characteristics of stream sediments soils and rocks in Banpo antimony mine area have been elucidated distribution peculiarities of macro elements micro elements and thermal released mercury content been summarized Element migration and accumulation during
·The antimony occurrences of the Iberian peninsula are described in terms of mineralogi cal associations geochemical features and chronostratigraphic distribution of the orebod ies
The Xikuangshan mine is situated in central Hunan China and is the largest antimony deposit in the world The mineralization is hosted in Middle Upper Devonian carbonate rocks Sm Nd isotope analysis of six calcite samples and one stibnite sample gives an isochron age of •}12 Ma with an initial 143Nd/144Nd ratio of and an ƒÃNn value of This age