物探与化探Issue(4)：660-666,7.DOI:10.11720/wtyht.2014.4.06
甘肃岗岔金矿3号矿脉原生晕分带特征及其找矿意义
Primary halo zoning of No. 3 ore vein in the Gangcha gold deposit of Gansu and its ore-proepecting significance
摘要
Abstract
Located in Luqu-Chengxian thrust nappe tectonic zone of Qinling orogenic belt, the Gangcha gold deposit is a typical tecton-ic alteration rock type gold deposit. The surface of the ore deposit controls five ore veins, which vertically extends for over 500 m, with their proven reserves reaching nearly 19 tons. Among them, the third vein is the largest gold vein, which extends almost in north-south direction, with an outcropped length of more than 1 km, an average grade of 2.99×10-6, and an average thickness of 2.91 m. Based on field investigation, the authors made an analysis of the geochemistry of various elements in relation to the ore veins. Combined with the association regularities of the general geochemical primary halo elements and the distribution characteristics of the single element con-trast, the authors determined the element combination characteristics of No. 3 ore vein as follows:Au-Ag-Pb-Zn is the near-ore hole el-ement association, Hg-As is the front halo element association, and Bi-Co-Cu-Ni is the rear halo element association. Based on the a-bove element association characteristics, the authors analyzed the primary halo of the third vein, and the result shows that the charac-teristics of the axial zonation and superposition are obvious, the mineralization of the vein has southward characteristics, and the super-imposed halo has not yet been closed in the extending direction. The authors thus infer that the good prospecting potential may exist in the southern depth of the ore deposit.关键词
原生晕/深部预测/构造蚀变/岗岔金矿/甘肃Key words
primary halo/deep forecast/altered rock type/Gangcha gold deposit/Gansu Province分类
天文与地球科学引用本文复制引用
鲍霖,申俊峰,曹卫东,薄海军,李金春,李可,王佳新..甘肃岗岔金矿3号矿脉原生晕分带特征及其找矿意义[J].物探与化探,2014,(4):660-666,7.基金项目
国家自然科学基金 （）
