杨振德, 张秀棋. 温杖子金矿成因类型与成矿模式[J]. 地质与资源, 1995, 4(2): 118-123.
    引用本文: 杨振德, 张秀棋. 温杖子金矿成因类型与成矿模式[J]. 地质与资源, 1995, 4(2): 118-123.
    Yang Zhende, Zhang Xiuqi. GENETIC TYPE AND METALLOGENETIC MODEL OF WENZHANGZI GOLD DEPOSIT, JIANCHANG COUNTY,LIAONING PROVINCE[J]. Geology and Resources, 1995, 4(2): 118-123.
    Citation: Yang Zhende, Zhang Xiuqi. GENETIC TYPE AND METALLOGENETIC MODEL OF WENZHANGZI GOLD DEPOSIT, JIANCHANG COUNTY,LIAONING PROVINCE[J]. Geology and Resources, 1995, 4(2): 118-123.

    温杖子金矿成因类型与成矿模式

    GENETIC TYPE AND METALLOGENETIC MODEL OF WENZHANGZI GOLD DEPOSIT, JIANCHANG COUNTY,LIAONING PROVINCE

    • 摘要: 温杖子金矿的形成经历了长期的成矿作用和多次矿化富集,具叠加成因特点,主要成因类型为侵入体接触带型和中低温热液型。成矿作用从晚侏罗世开始,一直持续到第三纪末,约延续了150Ma。

       

      Abstract: Wenzhangzi gold deposit is located in the south part of Jianchang county, Liaoning province, and tectonically, near the boundary between Shanhaiguan mega-uplift belt and west Liaoning dipression, In Proterozoic era, the ancient metamorphic rocks in the mining district were mostly changed into granites by fusion. There were intensive magmatic intrusions and eruptions in Mesozoic era. Due to thermodynamic activities, the strata of changcheng, Jixian, and Jurassic system, exposed in the gold mine, were undergone extensive alteration.

       

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