云南双柏大箐边锌铁矿矿床地质特征及矿床成因  

GEOLOGICAL CHARACTERISTICS AND GENESIS OF THE DAQINGBIAN ZINC-IRON DEPOSIT IN SHUANGBAI,YUNNAN

作　　者：姚顺列 朱观强 YAO Shun-lie;ZHU Guan-qiang(Yunnan Bureau of Nonferrous Geology,Kunming 650051)

机构地区：[1]云南省有色地质局,云南昆明650051

出　　处：《云南地质》2024年第S01期140-144,共5页Yunnan Geology

摘　　要：大箐边锌铁矿位于石羊场-太和街铅锌矿远景区内,矿体呈层状、似层状赋存于上三叠统白土田组碎屑岩层间构造破碎带中,矿体受地层、岩性、构造多因数控制,矿床成因类型为中-低温热液矿床。TheDaqingbian zinc-iron deposit is located within the Shiyangchang-Taihejie lead-zinc mineralization prospect area.The ore body is stratiform and quasi-stratiform,hosted in the interlayer structural fracture zone of the clastic rocks of the Upper Triassic Baitutian Formation,and is controlled by multiple factors,such as stratigraphy,lithology,and structure.The deposit is classified as a medium-lowtemperature hydrothermal deposit.

关 键 词：地层+岩性+构造控矿 中-低温热液矿床 大箐边锌铁矿 云南双柏 

分 类 号：P618.31[天文地球—矿床学] P618.43[天文地球—地质学]