Effection of WulanHada-Gaowusu fault to the hydrologic condition for uranium mineralization in Shangdu Basin

Effection of WulanHada-Gaowusu fault to the hydrologic condition for uranium mineralization in Shangdu Basin
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发表时间:
2006
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通讯作者:
Liu Qun-fang
Liu Qun-fang
中科院分区:
其他
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作者:
Liu Qun-fang

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商都盆地内可能存在长期活动的深大断裂,它对盆地的构造、上覆岩层、地下水动力场和地球化学环境都产生了影响,本文分析了深大断裂存在的证据,阐述了深大断裂对潜在砂岩型铀存款成矿的影响。
Within the basin of Shangdu,there may occured deep-large fault of long activiation which had affected the basin in its structure,lithofaces of the overlays,dynamic field of undergroud water and the environment of geochemistry.This paper makes analysis on the evidence of the deep-large fault and elaborates its affection to the mineralization of potential sandstone type uranium deposit.