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矿床地质  2003 

甘肃桦树沟铜矿床成矿年龄讨论

Keywords: 地球化学,铜矿床,成矿年龄,甘肃,桦树沟

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Abstract:

桦树沟铜矿床是近年来在北祁连山西段镜铁山矿田发现的一种新类型铜矿床。作者在矿床区域地质背景、地质特征分析的基础上,通过对与成矿密切相关的石英闪长岩脉中的锆石U-Pb同位素年龄及蚀变岩型铜矿石的40Ar-39Ar同位素年龄测定,认为桦树沟铜矿床是在元古宙铜预富集的基础上,富含铜元素的条带状铁建造经加里东造山期的挤压、破碎,隐伏花岗岩基和石英闪长岩脉侵入及与衍生成矿流体的水岩反应等作用,使其中的铜元素活化析出并被带到就近的有利构造空间沉淀成矿,其成矿年龄限定于(364.7±8.4)Ma~(476±15)Ma之间。

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