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。
As a result, Kamchatka has numerous hydrothermal systems, which constantly release geothermal gases and fluids out to the earth surface.
其众多的热液系统不断的向地表释放地热气体和流体。
The geothermal event of the end of the Late Devonian to the Carboniferous extensional deformation of basin superimposing of deep source hot fluids ( D 2);
2晚泥盆世-石炭纪伸展变形-深源热流体叠加事件(D2)。
The geothermal event of compression deformation of basin superimposing of hydrothermal fluids in the Indo Chinese orogen ( D 3);
3印支期挤压收缩变形-热改造事件(D3)。
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