Xikuangshan Mine

From Wikipedia, the free encyclopedia
Jump to: navigation, search

Xikuangshan mine (simplified Chinese: 锡矿山; traditional Chinese: 錫礦山; pinyin: Xīkuàngshān) in Lengshuijiang, Hunan, China,[1] contains the world's largest deposit of antimony.[2] It is unique in that there is a large deposit of stibnite (Sb2S3) in a layer of Devonian limestone. There are three mineral beds which are between 2.5 and 8 m thick which are folded in an anticline that plunges to the south-west. The total mineralised area of the mine has a surface extent of 14 km2. There are two different units at the mine, the northern one produces mixed oxide and sulfide such as stibiconite (Sb3O6(OH)) and the southern one produces stibnite. Ore is concentrated and refined on site in a refinery with a capacity of 10,000 tonnes of antimony per year.[3]

History[edit]

The mine is thought to have been discovered in 1521 and was originally mined for its tin deposits. 464,000 tonnes of antimony were produced at the mine between 1892 and 1929. From 1949 to 1981, 172,000 tonnes of antimony were produced. In 1981 1,700 tonnes of ore was being mined each day which was between 2 and 3 percent pure antimony.[3]

Reserves[edit]

In 1981, reserves at the Xikuangshan deposit amounted to 10,000,000 tonnes of ore that contained 2 to 3 percent antimony (200-300,000 tonnes of antimony), at the time geologists thought that there may be more in the area.[3] By 2002 the estimated size of the deposit was 2,110,000 tonnes of pure antimony.[4] The ore is composed of quartz, calcite, stibnite and some pyrite.[5]

Formation[edit]

Using Samarium-neodymium dating, it has been estimated that the deposit formed during the late Jurassic-early Cretaceous period (around 145 million years ago).[4]

Water Pollution[edit]

In April 2010 it was reported that antimony levels in water near the mine were as high as 11 parts per million, a thousand times those found in uncontaminated water. The antimony was found to be in the V oxidation state, believed to be the least dangerous aqueous form (antimony can have a I, III or V oxidation state). The environmental effects of this high level of the rare metal are poorly understood and are currently under investigation by a team from the Chinese Academy of Sciences, Indiana University Bloomington and the University of Alberta.

References[edit]

  1. ^ What's New in the Mineral World? Thomas P. Moore The Mineralogical Record
  2. ^ Penga, J. -T; R. Z. Hua and P. G. Burnardb (16 October 2003). "Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer". Chemical Geology 200 (1-2): 129–136. doi:10.1016/S0009-2541(03)00187-6. 
  3. ^ a b c Carter, W. D.; T. H. Kiilsgaard (1983). "Landsat analysis of the Yangjiatan tungsten district, Hunan Province, People's Republic of China". Advances in Space Research 3 (2): 113–123. Bibcode:1983AdSpR...3Q.113C. doi:10.1016/0273-1177(83)90110-2. 
  4. ^ a b Peng, Jiantang; Ruizhong Hu. Yuanxian Lin and Junhong Zhao (July 2002). "Sm-Nd isotope dating of hydrothermal calcites from the Xikuangshan antimony deposit, Central Hunan". Chinese Science Bulletin 47 (13): 1134–1137. doi:10.1360/02tb9254. 
  5. ^ Yang, Dong-sheng; Masaaki Shimizu, Hidehiko Shimazaki, Xian-hua Li and Qing-lin Xie (5 Nov 2008). "Sulfur Isotope Geochemistry of the Supergiant Xikuangshan Sb Deposit, Central Hunan, China: Constraints on Sources of Ore Constituents". Resource Geology 56 (4): 385–396. doi:10.1111/j.1751-3928.2006.tb00291.x. 

External links[edit]