Characteristics of two mafic-ultramafic rock series in the Xiangshan Cu-Ni-(V) Ti-Fe ore district, Xinjiang.
文献类型：期刊论文
| 作者 | Wang YuWang1,2; Wang JingBin1,2; Wang LiJuan1,2; Long LingLi1 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2009-04-01 |
| 卷号 | 25期号:4页码:888-900 |
| 关键词 | Mafic-ultramafic complex Cu-Ni rock series (V-) Ti-Fe rock series Xiangshan Xinjiang |
| ISSN号 | 1000-0569 |
| 文献子类 | Article |
| 英文摘要 | The mafic-ultramafic complex in the Xiangshan area of the eastern Tianshan Mts., Xinjiang, produce a medium-sized Middle-Xiangshan Cu-Ni deposit and a large-scale western-Xiangshan Cu-Ni-(V-) Ti-Fe deposit. Through systematical field investigation and sampling for the suit of mafic-ultramafic rocks, a detailed petrology and geochemistry research was carried out and two rock series with different metallogenetic specialization in study area have been identified. 1) Early stage rock series related to (V) -Ti-Fe mineralization with rock association of aplitic gabbro, Ti-Fe gabbro (Ti-Fe ore), Ti-bearing (homblende) gabbro and leucogabbro, shortly called as "(V-) Ti-Fe rock series". The three rock types of Ti-Fe ore, Ti-bearing gabbro and leucogabbro have continued evolution and gradual transition in mineral assemblage and rock texture. This series is characterized by alkali, Fe, Ti, Si, Al and Ca-rich, high calc-alkaline enrichment index (calk/in) and low mafic index (m/f) in chemical composition, and by distinct plagioclase cumulation and magma fractional crystallization in geochemistry of REE and trace elements. 2) Later stage rock series that can intrude in the Ti-Fe series rocks related to Cu-Ni sulfide mineralization with rock association of ultramafic rocks, rhythmic olive gabbro and altered hornblende gabbro, shortly called as "Cu-Ni rock series". This series is characterized by Mg-rich and relatively lower Fe, Ti, Si, Al, K and Na contents in chemical composition, and by gently REE and trace patterns that reflect a characteristics of primary mantle or depleted mantle. fire other hypabyssal dykes (diabase) in the ore district, mainly as later additional facies of gabbro, display an end evolution of the two rock series, i.e., product of magma mixing of two residual magma series. |
| WOS关键词 | CRYSTALLIZATION ; DEPOSITS ; SYSTEM |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000265945600013 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/71836]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Wang YuWang |
| 作者单位 | 1.Beijing Inst Geol Mineral Resources, Beijing 100012, Peoples R China 2.CAS, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang YuWang,Wang JingBin,Wang LiJuan,et al. Characteristics of two mafic-ultramafic rock series in the Xiangshan Cu-Ni-(V) Ti-Fe ore district, Xinjiang.[J]. ACTA PETROLOGICA SINICA,2009,25(4):888-900. |
| APA | Wang YuWang,Wang JingBin,Wang LiJuan,&Long LingLi.(2009).Characteristics of two mafic-ultramafic rock series in the Xiangshan Cu-Ni-(V) Ti-Fe ore district, Xinjiang..ACTA PETROLOGICA SINICA,25(4),888-900. |
| MLA | Wang YuWang,et al."Characteristics of two mafic-ultramafic rock series in the Xiangshan Cu-Ni-(V) Ti-Fe ore district, Xinjiang.".ACTA PETROLOGICA SINICA 25.4(2009):888-900. |
入库方式： OAI收割
来源：地质与地球物理研究所
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