浅海相
its wall rocks are a suit of shore to shallow sea facies carbonaceous carbonate and quartz sandstone formations.
围岩为一套滨海-浅海相富含碳质碳酸盐(石英砂岩)建造。
both of them are characterized by carbonate + clastic formation of shallow sea facies and filling sequence of transgression type.
都是以浅海相碳酸盐岩—碎屑岩沉积建造和海进型充填序列为特征。
Ore bodies developed in the the top of Doushantuo Formation ( Z1d) Which is shallow sea facies sedimentary dialogite deposits and the ore body in the stratified or stratoid, stable but often repeat or lost because of faults.
锰矿体赋存于陡山沱组(Z1d)顶部,为浅海相沉积菱锰矿床,锰矿体呈层状或似层状产出,层位稳定,其中常因断层重复或局部断失。
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