作者:WU Xiang-bin DAI Ta-gen WANG Zhi-bin FANG Sheng-kui
摘要:The Dachang tin-polymetallic ore field in northern Guangxi,China,lies in a mid-late Paleozoic rift that borders up the southern boundary of the Jiangnan-Xuefeng Massif.As a giant ore deposit,it deposited in middle of the Nandang-Hechi metallogenic zone.The orehosting strata are of the Devonion,which shows the evident characteristics of polymetallic elements,i.e: ,Sn,Zn,Pb,Sb,As,Cu,Ag,In,Ge,Cd,et al.,and over 1 000 000 t tin reserves.
发文机构:Institute of Geology Liouzhou Huaxi Co.Ltd.
分类号: P5[天文地球—地质学]