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辽宁黑水地区构造特征及其控矿作用

World Nuclear Geoscience(2009)

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Abstract
阐述了黑水地区区域构造新构造运动的演化特点,提出了目的层--孙家湾组沉积洼陷控矿和地下水的补-径-排主要通过断裂系统来完成,两组断裂交汇处为地下水从径流向排泄的转换部位,也是铀富集成矿部位.
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Key words
ore-control by sedimentary depression,structural features,Heishui area,Sunjiawan Formation
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