福建泰宁李家坊金矿地质特征与成因分析
Geology of Fujian(2011)
Abstract
泰宁李家坊金矿位于崇安—石城深断裂带中段,矿体是在区域变质、构造活动、岩浆侵入的长期作用下形成的,矿体主要贮存于中元古代交溪组混合岩化变质岩中,为断裂破碎带蚀变岩型金矿,主要成矿期为志留纪。
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Key words
Lijiafang,cause analysis,geological features,gold deposit
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