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宁陕县正河金矿床构造控矿特征及矿床成因初探

MINERAL RESOURCES AND GEOLOGY(2005)

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Abstract
通过对正河金矿的构造控矿特征、成矿物质来源及成矿作用的讨论,认为蚀变矿化带受控于次级背斜,为背斜核部的轴面劈理化带,山阳-凤镇深大断裂是该矿床的导矿构造.该矿床成矿作用经历了多期次的构造演化过程,成因为热水沉积-变质变形-构造热液改造型矿床.
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Key words
zhenghe gold deposit,deposit genesis,ore-controlling
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