Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.
沉积
金矿床的矿体是一些不连续的内
地质体,通常赋存于断裂带、角砾体层(性单位)中。
Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.
沉积金矿床的矿体是一些不连续的内地质体,通常赋存于断裂带、角砾体层(性单位)中。
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