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    燕建设, 王铭生, 杨建朝, 徐育新. 2000: 豫西马超营断裂带的构造演化及其与金等成矿的关系. 地质通报, 19(2): 166-171.
    引用本文: 燕建设, 王铭生, 杨建朝, 徐育新. 2000: 豫西马超营断裂带的构造演化及其与金等成矿的关系. 地质通报, 19(2): 166-171.
    shu
    2000: Tectonic evolution of the Machaoying fault zone in western Henan and its relationship with Au polymetallic mineralization. Geological Bulletin of China, 19(2): 166-171.
    Citation: 2000: Tectonic evolution of the Machaoying fault zone in western Henan and its relationship with Au polymetallic mineralization. Geological Bulletin of China, 19(2): 166-171.
    shu

    豫西马超营断裂带的构造演化及其与金等成矿的关系

    Tectonic evolution of the Machaoying fault zone in western Henan and its relationship with Au polymetallic mineralization

      摘要
    • 摘要: 马超营断裂带是豫西华北地台南缘一条重要的控矿构造带 ,具有复杂的构造演化史 ,至少发生过 5个旋回、7个世代的构造事件。其中海西—印支期的伸展滑脱构造体制和燕山期的逆冲推覆构造体制 ,对该构造带的发展演化和金、多金属成矿起着重要的作用。

       

      Abstract: The Machaoying fault zone is a major ore control tectonic belt along the southern margin of the North China platform in western Henan. Being complicated in structure, it was subjected to at least 7 tectonic events of 5 cycles. Among them, the Hercynian Indosinian extention decollement and the Yanshanian thrust napping played an important role in the evolution of the fault zone and the formation of Au polymetallic ore deposits.

       

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