横山岭铅锌矿床地球化学特征

来源期刊：中南大学学报(自然科学版)1991年第2期

论文作者：孙振家

文章页码：123 - 130

关键词：地球化学; 多因复成矿床; 铅锌矿; 横山岭

Key words：geochemistry; polygenetic compound ore deposits; lead-zinc deposits; Hengshanling

摘    要：文中讨论了横山岭铅锌矿床成矿元素地球化学背景、演化、空间分布特征及其富集过程,同时阐明本矿床为一受矿源层、矿源体、构造位控制的多因复成矿床。

Abstract: The geochemical setting, evolution, distribution, and mineralization proccesses of the ore-forming elements in Hengshanling lead-zinc deposits are presented and discussed in this paper. It is explained that the deposit is a polygenetic compound ore deposit which was controlled by source rocks and constructures' positions.