新疆和田长山沟汞矿床地质特征及成因研究  

Xinjiang and Tian Long Valley geological characteristics and genesis of mercury deposit

作　　者：曹佰迪[1] CAO Bai-di(Xi'an geological survey center of the China Geological Survey, Xi'an 710054,China)

机构地区：[1]中国地质调查局西安地质调查中心,陕西西安710054

出　　处：《世界有色金属》2018年第1期149-150,共2页World Nonferrous Metals

摘　　要：长山沟汞矿床位于新疆和田地区,矿区构造位置处于巴颜喀拉晚古生代-中生代边缘裂陷盆地西北缘。矿体赋存于中二叠世黄羊岭组地层中。经研究认为,该矿床为产于砂岩中的岩浆期后低温热液交代充填型脉状矿床。Changshan channel mercury deposit is located in Hetian area of Xinjiang,the tectonic location in the late Paleozoic Mesozoic rift basin in northwestern margin.The orebodies occur in the Middle Permian Huangyangling formation.It is considered that the deposit is a vein deposit of low temperature hydrothermal metasomatism after magmatic period in sandstone.

关 键 词：长山沟汞矿床 地质特征 

分 类 号：P618.68[天文地球—矿床学]