CAJ | 학술논문

三家子金矿位于冀东金成矿带东部，矿区内分布大量受断裂构造控制的含金石英脉，通过野外和室内研究，确定其成矿物质来源于燕山期岩浆期后热液。这些成矿热液在沿矿区内深大断裂F1向上运移过程中，部分成矿物质在F1断裂沿走向变化处发生沉淀，其它成矿物质在F1断裂派生的次级张裂隙中沉淀。该矿床属于受断裂控制的中低温、岩浆期后热液矿床。
삼가자금광위우기동금성광대동부，광구내분포대량수단렬구조공제적함금석영맥，통과야외화실내연구，학정기성광물질래원우연산기암장기후열액。저사성광열액재연광구내심대단렬F1향상운이과정중，부분성광물질재F1단렬연주향변화처발생침정，기타성광물질재F1단렬파생적차급장렬극중침정。해광상속우수단렬공제적중저온、암장기후열액광상。
Sanjiazi gold deposit is located in the eastern of gold metallogenic belt of the Eastern Hebei Province, widely developed mass auriferous quartz veins which were controlled by fault structure. We confirmed that the metallogenic materials derived from Yanshanian post-magmatic hydrotherm through wild researched and laboratory studied. Part of the metallogenic materials sedimented when the trend of fault F1 changed, while metallogenic hydrothermal were moved up along the deep fault F1, and other metallogenic materials sedimented in the secondary tensional fracture derived by fault F1. The Sanjiazi gold deposit belongs to the medium-lower temperature and post-magmatic hydrothermal deposit, which was controlled by fault.