• 责任者：Li Huan (Institute of Geology ; Central South University ; Changsha 410083 ; China) ; Xi Xiaoshuang
• 刊名：Geology and Prospecting
• 出版年：2011
• 卷期：47(3)
• 关键词：多金属矿 ; polymetallic ores ; 矿床成因 ; mineral deposit genesis ; 青海 ; Qinghai Province
• 页码：p.380-387
• 图表：3 illus., 3 tables, 22 refs.
• 分类号：1001
• issnNo：ISSN0495-5331
• isbnNo：CN11-2043/P

The Zhaokalong iron-copper-polymetallic deposit was produced in the back-arc rift sedimentary basin during the Late Triassic, with mineralization of iron, copper, gold, lead, zinc and other metallic ores. Ore bodies lie in the clastic rock of the upper Batang Group of Triassic, strictly controlled by the stratigraphy and lithology. According to the generation environment of the deposit, the classification of volcanic rocks, structural characteristics of ore bodies and the ore occurrence form, it can be preliminarily concluded that this deposit is an iron oxide-sulfide iron-copper-polymetallic deposit related to seafloor exhalation.