秦岭型铅-锌矿床  

THE QINLING-TYPE LEAD AND ZINC ORE DEPOSIT

作　　者：李健中 何典仁 吴健民[3] 

机构地区：[1]甘肃有包金属地质研究所 [2]西北有色地质勘探公司地质研究所 [3]中国有色金属工业总公司矿产地质研究院

出　　处：《地质学报》1992年第3期257-268,共12页Acta Geologica Sinica

摘　　要：秦岭型铅-锌矿床是产于北秦岭华力西褶皱系泥盆纪地层中,由海相碳酸盐岩及细碎屑岩系容矿的热水沉积-改造型铅-锌矿床。它可进一步划分为热水沉积矿床(厂坝式)及热水沉积改造矿床(毕家山-铅硐山式)两个亚类。与世界古生界著名铅-锌矿床对比,它包括了热水沉积矿床(Meggen型)和热水改造矿床(Mississippi Valley型)的一些特征,但又有别于它们成为一个独立类型。The Qinling-type lead and zinc ore deposit is located in the Qinling fold belt, occurring in the Devonian marine fine clastic and carbonate rocks. It is a sedimentary-reworked ore deposit which is basically a sedimentary deposit further hydrothermally reformed. It may be separated into two subtypes: one is the sedimentary ore deposit (Changba subtype); and the other is the sedimentary-reworked ore deposit (Bijiashan-Qiandongshan subtype).In comparison with some famous lead and zinc ore deposits in the world which occur also in Palaeozoic formations, it seems evident that the Qinling-type lead and zinc deposit is an important transitional type between the Meggen-type and the Mississipi type.

关 键 词：铅锌矿 矿床 秦岭型 

分 类 号：P618.420.2[天文地球—矿床学]