CAJ | 학술논문

蔡凹锑矿床位于北秦岭加里东造山带内，产于古元古代秦岭群地层中，严格受区域性大断裂和界岭复式背斜两翼的次级褶皱和断裂控制。文中从分析成矿地质背景、矿床地质特征和矿床成因入手，总结了矿床的控矿因素，认为该矿床受含矿地层、构造和岩浆岩等因素控制；提出了新的找矿方向，认为蔡凹锑矿床深部仍有较大的找矿潜力，围绕有利的构造部位和矿化蚀变标志追索矿体，实现找矿勘查的突破。
채요제광상위우북진령가리동조산대내，산우고원고대진령군지층중，엄격수구역성대단렬화계령복식배사량익적차급습추화단렬공제。문중종분석성광지질배경、광상지질특정화광상성인입수，총결료광상적공광인소，인위해광상수함광지층、구조화암장암등인소공제；제출료신적조광방향，인위채요제광상심부잉유교대적조광잠력，위요유리적구조부위화광화식변표지추색광체，실현조광감사적돌파。
Caiwa antimony deposit in Shanxi province locates in the northern Qinling Caledonian fold beit. It oc-curred in metamorphic rocks of Proterozoic Qinling group, and is strictly controlled by secondly folds of regional fault and faults of Jieling anticlinorium. Based on comprensive analysis of metallogenic geological setting, geological characteristics and the origin of deposit, ore-controlling factors of this deposit have been summarized. It is regar-ded that the Caiwa antimony deposit are obviously controlled by ore-bearing strata, faults and magmatism. New prospecting direction is proposed. It is inferred that there is prospecting potentiality in the deep part of Caiwa anti-mony deposit. Based on favorable faults position and the ore prospecting indicators of mineralization and alteration, new orebodies can be found and a great breakthrough in ore prospecting can be gained.