CAJ | 학술논문

乔端金矿床位于区域性乔端-瓦穴子断裂上盘的次级构造带中，矿体赋存于加里东期石英闪长岩中。矿床矿石类型包括蚀变岩型和石英脉型两种；矿床严格受构造破碎带控制，成因上与燕山期岩浆侵入活动关系密切。
교단금광상위우구역성교단-와혈자단렬상반적차급구조대중，광체부존우가리동기석영섬장암중。광상광석류형포괄식변암형화석영맥형량충；광상엄격수구조파쇄대공제，성인상여연산기암장침입활동관계밀절。
The Qiaoduan gold deposit is located in the secondary structural belt appearing in the hanging wall of Qiaoduan-Waxuezi regional fault. The ore body mainly occurs in Caledonian Quartz diorite. There are two major ore types, namely, altered rock type and quartz vein type. The deposit is strictly controlled by structural fracture zone, and closely related to Yanshanian magma intrusion activities in genesis. In this paper, we studied the regional geological background and geological features of the Qiaoduan gold deposit, and then discussed the genesis.