丹东万宝源钼矿成因探讨

宽甸万宝源钼矿是比较典型的中等规模斑岩钼矿床，产于燕山期石柱子花岗闪长岩及石英斑岩中，品位高、厚度大，在国内同类成因钼矿具有一定的代表性，经同位素测定，万宝源钼矿的成矿流体来自于深源岩浆或上地幔中酸性深源浅成侵入斑岩体。属于“同源多体”的同一成矿系列。成矿期为燕山期，是典型的岩浆期后浅成中温热液矿床。

Dandong Wanbao Source Origin of Molybdenum

Kuandian Wanbao molybdenum Mine is a more typical mid--sized porphyry molybdenum deposit, produced in the sub--pillars Yanshanian granodiorite and quartz porphyry in the high--grade, thickness, and in the domestic similar molybdenum causes a certain representation, measured by isotope, Wanbao source molybdenum of ore--forming fluids from the deep source of magma or deep source of mantle--acid hypabyssal porphyry intrusion. Are ＂homologous multi--body＂ of the same metallogenic series. Yanshanian period of mineralization is a typical post--magtrmtic epithermal.