内蒙古黄岗梁-乌兰浩特锡铅锌铜多金属成矿带成矿机制及时空架构

    Ore-forming mechanism and the temporal and spatial structure of the Huanggangliang-Wulanhaote tin-lead-zinc-copper-polymetallic metallogenic belt,Inner Mongolia

    • 摘要: 黄岗梁-乌兰浩特锡铅锌铜多金属成矿带,地处内蒙古东南部,近北东走向,长约400km,是铜、铅、锌、锡、银等多金属矿产的集中分布区。本文在综合前人研究的基础上,对研究区的区域成矿地质背景、成矿时空特征、成矿条件与成矿机制进行了探讨,总结出3个矿床成矿系列9个矿床式。

       

      Abstract: Huanggangliang-Wulanhaote tin-lead-zinc-copper-polymetallic metallogenic belt is located in the southeastern part of Inner Mongolia. Near the North East direction, about 400km, is the copper, lead, zinc, tin, silver and other metal mineral concentration distribution. In this paper, a comprehensive basis of previous studies, the study area on the regional metallogenic geological setting, ore-forming space-time characteristics of ore-forming conditions and ore-forming mechanisms are discussed, summed up the three metallogenic series and 9-style deposit.

       

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