新疆东昆仑屈库勒克东金锑矿床构造叠加晕特征及深部找矿预测  

Structural Superimposed Halo Characteristics and Deep Prospecting Prediction of Qukulek East Gold(Antimony)Deposit in East Kunlun,Xinjiang

作　　者：刘兵 连政 陈威 郑鸿 Liu Bing;Lian Zheng;ChenWei;Zheng Hong(Regional Geological Survey Center of Xinjiang Uygur Autonomous Region Geological Bureau,Urumqi,Xinjiang,830013,China)

机构地区：[1]新疆维吾尔自治区地质局区域地质调查中心,新疆乌鲁木齐830013

出　　处：《新疆地质》2025年第1期54-60,共7页Xinjiang Geology

基　　金：自治区重点研发项目(2023B03016-2);自然资源部新一轮找矿突破战略行动科技支撑项目(ZKKJ202427);国家科技重大专项项目(2024ZD1001802)共同资助。

摘　　要：东昆仑屈库勒克东金(锑)矿产于哈拉米兰河群上组岩层内,矿体受断裂破碎带控制。对Ⅰ2号矿体赋矿破碎蚀变带构造叠加晕特征进行研究,总结了赋矿破碎蚀变带多元素组合特征,确定了矿体前缘晕、近矿晕和尾晕分布特点,据流体成分不同和活动时间先后顺序划分为4个成矿阶段;建立了深部隐伏矿体预测的构造叠加晕模型,圈定了找矿预测区。The gold(antimony)deposit in qukulek East of East Kunlun is located in the upper group of Halamilanhe group,and the ore body is controlled by the fracture zone.Based on the study of the structural superimposed halo characteristics of the ore-bearing fractured alteration zone of No.I2 ore body,the multi-element combination characteristics of the ore-bearing fractured alteration zone are summarized,and the distribution characteristics of the front halo,near-ore halo and tail halo of the ore body are determined.According to the different fluid composition and the sequence of activity time,it can be divided into four metallogenic stages.The structural superimposed halo model for the prediction of deep concealed ore bodies was established,and the prospecting prediction area was delineated.

关 键 词：金矿 构造叠加晕 深部预测 屈库勒克东 

分 类 号：O614.123[理学—无机化学] O614.531[理学—化学]