蔡凹锑矿位于陕豫锑矿带的西段,为矿带中典型的锑矿床。 其控矿岩系主要为秦岭群中部雁岭沟组石墨大理岩。
The Caiwa middle - sized antimony deposit is located on the western Shanxi-Henan antimony ore belt, The hosting rocks are Yanlinggou Formation graphite marble of the Qinling Group.
在化学成份上,蔡家岭组火山岩不属于钾玄岩系列。
The petrochemical type of the Caijialing volcanic rocks couldn't belong to the potassic basaltic rock series.
在化学成份上,蔡家岭组火山岩不属于钾玄岩系列。
The petrochemical type of the Caijialing volcanic rocks couldn't belong to the potassic basaltic rock series.
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