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赵卡隆矿区位于青海玉树南部,是我国著名的三江成矿区的最具代表性的重要矿床,因为该地区地质较为复杂,并且地理位置偏远,给勘探工作带来很大的阻碍,勘探工作进程较为缓慢,但是经过多年的勘探,以发现这一地区的铁铜多金属矿具有一定的规模,并且显示出一定的成矿规律。为了更好的指导该区的找矿勘探工作,在深入研究该区域矿床成矿地质因素的前提下,探寻矿床的成矿规律。本文通过阐述地层构造型式和地层划分,总结成矿规律。
Located in the south of Yushu in Qinghai Province, Zhakailong mine is the most important and representative deposit in the famous Sanjiang mineralization area in our country. Due to its complex geology and remote location, the Zhakarong mining area has greatly hindered the exploration and exploration work More slowly, but after years of exploration to find that the area of iron-copper polymetallic ore has a certain scale, and shows a certain metallogenic regularity. In order to better guide exploration and prospecting work in the area, on the premise of deeply studying the mineralization geological factors of the ore deposits in this area, the metallogenic regularity of the ore deposits is probed. This article summarizes the ore-forming rules by describing the stratigraphic structure and stratigraphic division.