次级破裂
Three-class controLing system consists of the regional tectonic setting, regional ore-control faulted structures and subsidiary host fracture structure.
从该区所具有的区域构造环境至区域控矿断裂构造到次级容矿裂隙构造,构成了三级控矿系统。
Regional deep-fault is the main pathway for meteoric water and geothermal fluids, subsidiary fracture is ore depositing structures, and fault tectonite are the main host rocks.
区域性深大断裂是沟通天水和地热流体的主要通道,次级断裂是矿体的储矿构造,脆性粗碎屑岩和火山碎屑岩(沉积火山岩)构成的断裂构造岩是主要的容矿岩石。
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