Sediments of channel debris flow facies, is generally well developed in limnic fault basin and forms the important geological factors that influence the mining.
在陆相含煤断陷盆地，煤层中的河道泥石流相沉积通常比较发育，并成为影响采煤生产的重要地质因素。
Sediments of channel debris flow facies, is generally well developed in limnic fault basin and forms the important geological factors that influence the mining.
在陆相含煤断陷盆地，煤层中的河道泥石流相沉积通常比较发育，并成为影响采煤生产的重要地质因素。
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