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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。
The Machaoying fault zone is an important ore-controlling tectonic belt on the southern margin of the North China platform in the west of Henan Province. It has a complex tectonic evolution history and at least five cycles of gyration and seven generations of structural events have occurred. Among them, the Hercynian-Indosinian extensional detachment system and the Yanshanian thrust nappe structure system play an important role in the development and evolution of the structural belt and gold and polymetallic mineralization.