• 责任者：Zou Tao (Faculty of Land Resource Engineering ; Kunming University of Science and Technology ; Kunming 650093 ; China) ; Wang Jingbin
• 刊名：Geology and Prospecting
• 出版年：2011
• 卷期：47(5)
• 关键词：斑岩钼矿床 ; porphyry molybdenum deposit ; 斑岩铜矿床 ; porphyry copper deposit ; 矿床成因 ; mineral deposit genesis ; 内蒙古 ; Inner Mongolia
• 页码：p.737-747
• 图表：2 illus., 1 table, 16 refs.
• 分类号：1001
• issnNo：ISSN0495-5331
• isbnNo：CN11-2043/P

The Aolunhua mine is a large-scale porphyry Mo-Cu deposit. The ore mineral consists of molybdenite, chalcopyrite, pyrite, sphalerite, and galena.The major elements of the Aolunhua rock show high SiO₂, Al₂O₃, K, Na contents, with ratio of Na₂O/K₂O between 1.1～2.1, the value of σ between 3～3.7, and the ratio of A/CNK less than 1 (0.68～0.82). The lithology of Aolunhua rock is granodiorite-porphyry, belongs to Na-rich and K-high calc-alkaline rock series.Hydrothermal alterations in Aolunhua roughly shows zonation of quartz-K feldspathization, quartz-sericite, hornfelsed. Characteristics of mineral deposit geochemistry, field geological observations and petrological evidence suggest that the Aolunhua deposit is a porphyry type hypothermal-mesothermal molybdenum deposit. Evolution of magmatic and sulfur isotope show that mineralization is closely related to acidic porphyry and affected by mantle-derived magma mixing.