CAJ | 학술논문

　　双泉金矿是东准噶尔卡拉麦里成矿带上一个中型的与韧性剪切带有关的变质热液型金矿，赋矿地层为下石炭统南明水组，矿石主要类型为蚀变岩型。在漫长地质演化过程中，形成的构造模式、沉积环境、岩浆演化等，为双泉金矿的形成提供了有利条件。对成矿构造、成矿环境、物探、化探异常等条件进行归纳总结，建立了双泉金矿成矿模式，以期指导该成矿带上其它韧性剪切带型矿床的研究合找矿工作。
　　쌍천금광시동준갈이잡랍맥리성광대상일개중형적여인성전절대유관적변질열액형금광，부광지층위하석탄통남명수조，광석주요류형위식변암형。재만장지질연화과정중，형성적구조모식、침적배경、암장연화등，위쌍천금광적형성제공료유리조건。대성광구조、성광배경、물탐、화탐이상등조건진행귀납총결，건립료쌍천금광성광모식，이기지도해성광대상기타인성전절대형광상적연구합조광공작。
Shuangquan gold mine is located in East Junggar metallogenic belt,it is a medium-sized metamorphic hydro-thermal type gold mine related to a ductile shear zone,its ore formation is Lower Carboniferous Nanmingshui formation, and the main type of ore is alteration rocks.The tectonic pattern,sedimentary environment and the magatic evolution formed in the long geological evolution process,provide favorable condition for the formation of Shuangquan gold mine. After summarized the minerogenetic structures,metallogenic environment,geophysical,geochemical anomalies and so on, established Shuangquan gold metallogenic model in order to guidance other ductile shear zone type deposits in this metallogenic belt.