Ore bodies lie in the clastic rock of the upper Batang Group of Triassic, strictly controlled by the stratigraphy and lithology.
矿体赋存于三叠系巴塘群上部碎屑岩组上岩性段地层中，严格受地层和岩性控制。
The natural soda water occurs mainly in the pore-fissure confined aquifer of the clastic rock of Nenjiang group, Upper Cretaceous.
天然苏打水主要赋存于上白垩统嫩江组碎屑岩孔隙裂隙承压含水层中。
It has been proved that the clastic rock not only provide Pb and Zn for the deposits but also channeled the ore fluids during mineralization.
它们不但为矿床的形成提供了成矿金属，而且由于渗透率较大而为成矿流体的大规模侧向流动提供了通道。
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