【摘要】 矿区出露地层为震旦-寒武系浅变质岩。钼矿床与燕山期高氟、高锂的细粒少斑黑云母花岗岩和花岗斑岩存在密切的空间、时间关系,钼矿化赋存在岩体的内外接触带,包括含辉钼矿萤石石英脉,含辉钼矿的裂隙脉和蚀变岩石(云英岩化)内浸染状产出的钼矿化,含辉钼矿的萤石石英脉是受NEE-SWW向和近SN向裂隙带控制,构成矿床的富矿体,矿区内的富矿作用为钾长石化、黑云母化、云英岩化、萤石化、硅化、绢云母化和绿泥石化,其中,与钼矿化关系密切的蚀变作用是黑云母化、云英岩化、萤石化和硅化。更多还原

【Abstract】 The exposed strata of this ore area is Sinian-Cambrian epimetamorphic rocks.There is a close spacial and time relationship between the Mo deposit and the Yanshanian biotite granite with granite porphyry which present in fine grains with a few speckles and contain high F,high Li.The Mo mineralization,including the molybdenite-bearing fluorite-quartz vein and molybdenite-bearing cranny vein with the disseminating Mo mineralization in alteration rocks(greisenization),occurred in the inner and outer contacting zones of the rockbodies.The molybdenite-bearing fluorite-quartz vein is controlled by NEE-SWW trend with near SN trend cranny zones,which has been constituted as a rich ore-bearing orebody. The alteration for ores enrichment in this area includes K-feldspathization,biotitization,greisenization,fluoritization,siliconization,sericitization and chloritization,of which the alteration effects of biotitization,greisenization,fluoritization and siliconization have a close relationship with the Mo mineralization.更多还原