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商丹三角地区花岗伟晶岩型铀矿成矿环境研究及远景评价
引用本文:万吉,高立宝,王莲香.商丹三角地区花岗伟晶岩型铀矿成矿环境研究及远景评价[J].铀矿地质,1992(5).
作者姓名:万吉  高立宝  王莲香
作者单位:西北地勘局203研究所,西北地勘局203研究所,西北地勘局203研究所
摘    要:花岗伟晶岩型铀矿是目前发现的一种新类型铀矿。这种矿床的晶质铀矿是从花岗岩浆分异出来的富铀岩浆中结晶而成的。下元古界秦岭群是成矿有利环境,韧性剪切带是控岩控矿的主要构造。这种类型铀矿在商丹三角地区的远景是可观的。

关 键 词:花岗伟晶岩型铀矿  成矿环境  韧性剪切带

METALLOGENIC ENVIRONMENTAL STUDY AND PROSPECT ASSESSMENT OF TIlE GRANITE-PEGMATITE-TYPE URANIUM DEPOSIT IN SHANGXIAN-DANFENG TRIANGLE AREA,SHAANXI
Wan Ji Gao Libao Wang Lianxiang.METALLOGENIC ENVIRONMENTAL STUDY AND PROSPECT ASSESSMENT OF TIlE GRANITE-PEGMATITE-TYPE URANIUM DEPOSIT IN SHANGXIAN-DANFENG TRIANGLE AREA,SHAANXI[J].Uranium Geology,1992(5).
Authors:Wan Ji Gao Libao Wang Lianxiang
Abstract:The granite-pegmatite-type uranium deposit is a new type of uranium deposit which has been recently discovered. Uraninite in this type of deposit is crystallized by U-rich magma which is differentiated from granitic magma. The Qinling Group of Lower Proterozoic is an advantageous environment for metallogenesis and the ductile shear zone is a major structure to control rocks and ores. It is held that the prospect of the type of uranium deposit in Shangxian-Danfeng triangle area is considerable.
Keywords:Granite-pegmatite-type uranium deposit  Metallogenic environment  Ductile shear zone  
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