clastic eluvial ore deposit 碎屑残积矿床
Of the ore types in the Dongshengmiao polymetallic sulfide deposit, the clastic type is an important one of them.
碎屑型矿石是东升庙多金属硫铁矿床的主要矿石类型之一。
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。
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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