矿床为构造破碎斑岩蚀变型金矿床。
The deposit is a structure zone porphyry alteration type gold deposit.
矿石类型主要为蚀变砂岩型和构造破碎蚀变岩型。
The ores are mainly altered sandstone and tectonoclastic altered rock.
由于构造破碎和河流切割引起岩石卸荷与松动，使岩石有利于水的渗入和岩溶作用。
Due to the unloading and loose - ning brought about by tectonic shattering and river cutting, the mud limestone becomes favorable for water infiltration and karstification.
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