Citation: | ZHANG Kai, GOU Rong-tao, LIU Shu-lin, GUO Gang, XU Jun-jie, WANG Bo-wen, LI Hua-nan, YUAN Jing. CHARACTERISTICS AND SIGNIFICANCE OF THE COPPER-GOLD-ANTIMONY DEPOSITS IN DAGANGOU AREA, EAST KUNLUN[J]. Journal of Geomechanics, 2012, 18(4): 401-409. |
The East Kunlun area is located at the suture zone of Sino-Korean Plate, Tarim-Qaidam Plate, Yangtze Plate and India Plate. The special tectonic structural location decided its tectonic evolution being very complicated and distinctive. The geochemical anomalies in this area composed by Au-Co-Cu-Pb-Zn-Hg-Sb-As elements and most of them have been confirmed as anomalies related to mineral deposit. 198 ore deposits and ore spots have been found in this area. This showed a favorable ore-searching prospect. Total 6 ore deposits were discovered at Dagangou zone, including a copper multi-metal mineral belt and a gold-antimony ore-bearing structural alteration belt. Their mineralization characteristics are basically same. The ore deposit occurred in the Middle Triassic Naocangjiangou Formation west-northwest brittle-ductile shear zone and ashen-gray calcite quarts vein at the both sides of shear zone.
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Tectonic map of East Kunlun Mountain area
A sketch map showing the distributions of regional minerals
Characteristics of the copper-bearing quartz vein at the first period of mineralization
Characteristics of the copper-bearing quartz vein at the second period of mineralization
Characteristics of the antimonite ore produced in quartz and calcite veins
Characteristics of the antimonite ore produced in thin limestone
Characteristics of surface alteration and mineralization of the gold ore