菱锰矿;
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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