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乌岙铅锌矿床地球化学特征及其成因的讨论
引用本文:徐外生,刘崇民,周俊法,方原勤.乌岙铅锌矿床地球化学特征及其成因的讨论[J].物探与化探,1987,11(6):443-455.
作者姓名:徐外生  刘崇民  周俊法  方原勤
作者单位:地矿部物化探研究所 (徐外生,刘崇民),浙江省地矿局第七地质大队 (周俊法),浙江省地矿局第七地质大队(方原勤)
摘    要:本文借助于多种测试分析资料,在充分地研究矿区与成矿作用有关的岩石、矿石和矿物等地球化学特征的基础上,利用已获的研究成果,有说服力地进行了对比总结.尝试应用地球化学资料,讨论了矿床形成的矿质来源、控矿因素,以及沉淀富集条件等.指出该矿床应属岩浆热液型铅锌矿床.


GEOCHEMICAL CHARACTERISTICS OF THE WUAO Pb-Zn DEPOSIT AND ITS GENESIS
Institution:1. Institute of Exploration Geophysics and Geochemistry, MGMR;
2. No. 7 Geological Party, Bureau of Geology and Mineral Resources of Zhejiang Province
Abstract:With the help of analytic data obtained by various means, a thoroughinvestigation was conducted on geochemical characteristics of rocks, ores and minerals related to mineralizations in the ore district. On the basis of the results acquired in the research, this paper makes a convincing comparison and summarization and, using geochemical data, deals tentatively with sources or ore materials, ore-controlling factors and conditions for ore precipitation and enrichment during the formation of the ore deposit. It is indicated that this deposit is genetically a magmatic hydro thermal type Pb-Zn deposit.
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