摘要
鱼池岭钼矿属于超大型斑岩钼矿床.通过对区域地质背景、鱼池岭钼矿床地质特征和辉钼矿Re-Os同位素测年等研究,进而查明了鱼池岭钼矿床的含矿岩体特征、成因类型,分析了成矿物质的可能来源,厘定了成岩成矿年龄,并探讨了矿床成因.
Yuchiling molybdenum ore deposit belongs to the ultra-large porphyry molybdenum ore deposit. We studied the regional geology background,the Yuchiling molybdenum ore deposit geological characteristics,and the molbdenite Re-Os isotope deting,then we found out Yuchiling molybdenum deposit ore rock body characteristic, the origin type. We analyzed the mineralization material possible origin,defined the diagenetic metallogenic age, and discussed the causes of ore deposits at last.
出处
《河南科学》
2014年第4期600-604,共5页
Henan Science
基金
国土资源部公益性行业科研专项项目(20111107-2)
关键词
斑岩型钼矿床
地质特征
矿床成因
找矿方向
porphyry Mo deposit
geological characteristics
ore genesis
prospecting direction
