CAJ | 학술논문

栾川县石宝沟钼矿床位于华北地台南缘与秦岭褶皱系相交部位，在研究区域地质、矿区地质基础上，重点对矿床地质特征进行了研究，认为矿体形态、产状受花岗斑岩岩体形态、围岩岩性、构造控制较为明显，通过对矿床成因的分析，说明石宝沟钼矿床在空间上、时间上、成因上均与深部花岗岩浆有关，矿床成因应为斑岩-矽卡岩型，对以后寻找类似矿床有一定的借鉴意义。
란천현석보구목광상위우화북지태남연여진령습추계상교부위，재연구구역지질、광구지질기출상，중점대광상지질특정진행료연구，인위광체형태、산상수화강반암암체형태、위암암성、구조공제교위명현，통과대광상성인적분석，설명석보구목광상재공간상、시간상、성인상균여심부화강암장유관，광상성인응위반암-석잡암형，대이후심조유사광상유일정적차감의의。
Shibaogou molybdenite deposit from Luanchuan country is located in the intersection between south mar-gin of North China and Qinling fold system.Based on the research of regional and mineral geology,this article puts a special stress upon the deposit’s geological features research;we think that morphology and occurrence of the de-posit are clearly controlled by the morphology of granite -porphyry,lithological characters and contracture of the surrounding rock.Through preliminary analysis on the causes of the deposit,it shows that Shibaogou molybdenite deposit has a close relationship with the deep granitic magma,no matter on the cause of space,time and reasons;the ore genesis of the deposit could be porphyry-skarn,which provides certain significance on exploring such simi-lar deposit.