摘要
对西范坪斑岩铜矿的蚀变作用、流体包裹体特征等进行了研究,指出该矿床是由两期岩浆流体叠加作用所形成的。西范坪式斑岩型铜矿与喜山期中酸性岩浆侵入活动关系十分密切。根据斑岩铜矿床的成矿地质背景、矿床地质特征,探讨该铜矿的控矿条件、成矿机制。在总结成矿规律的基础上,进行资源预测,估算了资源量。
the alteration and fluid inclusion characteristics of Xifangping porphyry copper deposit are studied. It is pointed out that the deposit was formed by two periods of magmatic fluid superposition.The Xifangping porphyry copper deposit is closely related to the acid magmatic intrusion in the Himalayan period.According to the metallogenic geological background and geological characteristics of porphyry copper deposit, the ore-controlling conditions and metallogenic mechanism of the copper deposit are discussed.On the basis of summarizing the metallogenic law, the resources are predicted and the amount of resources is estimated.
引文
[1]侯增谦,莫宣学,杨志明,王安建,潘桂棠,曲晓明,聂凤军.青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型[J].中国地质.2006(02)
[2]付芳,杨铸生,赵丽琴.西范坪式斑岩型铜矿的成矿规律与预测资源量[J].四川地质学报.2014(01)