• 责任者：Liu Shentai (Tibet Yulong Copper Company Limited ; Changdu 854000 ; China) ; Lü Xinbiao
• 刊名：Acta Geoscientica Sinica
• 出版年：2012
• 卷期：33(2)
• 关键词：铜矿 ; copper ores ; 锌矿 ; zinc ores ; 稀土元素 ; rare earths ; 微量元素 ; minor elements ; 新疆 ; Xinjiang
• 页码：p.197-208
• 图表：6 illus., 5 tables, 25 refs.
• 分类号：1001
• issnNo：ISSN1006-3021
• isbnNo：CN11-3474/P

The Xiaorequanzi Cu(Zn) deposit of Xinjiang is located in the late Paleozoic island-arc of Danan Lake area, its ore bodies are hosted in a sedimentary rock suite of tuffaceous detritus, and its ore types are mainly massive chalcopyrite, sphalerite and other lodes. Based on a comparison of microstructures as well as distribution patterns of REE and trace elements between these sulfides, the authors hold that chalcopyrite has a better flowability than sphalerite, and the chalcopyrite tended to become active and move more easily than sphalerite under tense shear strain, and large-scale movement would lead to the concentration of chalcopyrite and finally the formation of the Xinjiang Xiaorequanzi Cu(Zn)deposit.