The Qulong copper porphyry deposit discovered in recent years is likely to develop into a superlarge copper porphyry deposit. The ore district has abundant surface water. There is a malachite precipitation zone several kilometers in length along the lower reach of the main water system in the ore district. This paper has discussed the main factors controlling the accumulation of malachite, the variation of element content in the water system before and after the rainy season and the indication role of hydrogeochemical anomalies in determining the position of the ore deposit and the perspective target area.
杨少平, 孔牧, 刘应汉, 刘华忠, 张学君, 董广法, 罗永平. 西藏驱龙铜矿区水地球化学特征及其对铜矿化指示作用[J]. 物探与化探, 2006, 30(6): 509-512.
YANG Shao-ping, KONG Mu, LIU Ying-han, LIU Hua-zhong, ZHANG Xue-jun, DONG Guang-fa, LUO Yong-ping. HYDROGEOCHEMICAL CHARACTERISTICS OF THE QULONG COPPER ORE DISTRICT IN TIBET AND THEIR INDICATION SIGNIFICANCE TO COPPER MINERALIZATION. Geophysical and Geochemical Exploration, 2006, 30(6): 509-512.