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哈密活水泉铁矿地质特征及找矿标志

张佳儒

XINJIANG YOUSE JINSHU（2018）

Cited 0|Views9
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Abstract
哈密活水泉铁矿位于哈尔里克古生代复合岛弧带,产于华力西中期中粗粒黑云母花岗岩体近南北向构造破碎带中,矿体受构造破碎带控制,构造破碎带为矿体赋存空间,由晚期岩浆结晶分异含铁热液沿断裂充填而成,为典型的岩浆热液型铁矿床.
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