摘要
云南省罗平县鑫鑫铅锌矿区内的矿体赋存于二叠系中统阳新组(P2y)浅灰色灰岩与青灰色、灰黑、灰白色白云岩互层的岩性中,受断裂裂隙构造及地层控制。
The orebodies in Xinxin Lead-Zinc Mine, Luoping County, Yunnan Province occur in the lithology of the interbedded light grey limestone and grey, grey-black and grey-white dolomite of the Yangxin Formation(P2 y) of the Permian System, which are controlled by fracture structure and strata.
引文
[1]贵州省革命委员会地质局.1:20万盘县区域地质调查报告[R].1973.
[2]司荣军.云南省富乐分散元素多金属矿床地球化学研究.2005.
[3]云南华联矿产勘探有限责任公司.云南省罗平县富乐镇鑫鑫采矿厂铅锌矿资源储量核实报告[R].2014.
[4]云南省有色地质局三一七队.云南省罗平县拖牛铅锌矿勘查阶段报告[R].2018.