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Petrogenesis of the Yangzhuang Nb- and Ta-rich A-type granite porphyry in West Junggar, Xinjiang, China
Wei Mao; Xiaofeng Li; Guo Wang; Rong Xiao; Mou Wang; Yanlong Li; Manchuan Ren; Yanping Bai; Feng Yang
2014
发表期刊Lithos
卷号198 -199期号:1页码:172-183
摘要West Junggar is featured with a wide spread of Late Carboniferous-Early Permian A-type granites. Systematic comparison of the Yangzhuang granite porphyry and the regional coeval A-type granites (RCAG) shows that: (1) all the Late Carboniferous-Early Permian A-type granites are of the A(2) group except the Yangzhuang granite porphyry; (2) the Nb and Ta contents of the Yangzhuang granite porphyry are nearly 10 times that of the RCAG while Ti content is more depleted; (3) epsilon Nd (t) of the Yangzhuang granite porphyry is slightly lower and the Sr isotope has a wider range relative to the RCAG. Previous research revealed that highly incompatible elements including Nb and Ta can be transferred into the mantle wedge by precipitation of amphibole from the ascending fluids generated by dehydration of subducted slab. It is inferred that enhanced heat flux brought by the Late Carboniferous ridge subduction decomposed amphibole in the mantle wedge to generate Nb and Ta-rich melt and finally produced the Yangzhuang granite porphyry.
关键词Yangzhuang Granite Porphyry A-type Granite Nb Ta Ridge Subduction West Junggar
学科领域矿床地球化学
收录类别SCI
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/352002/5235
专题矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
矿床地球化学国家重点实验室
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GB/T 7714
Wei Mao,Xiaofeng Li,Guo Wang,et al. Petrogenesis of the Yangzhuang Nb- and Ta-rich A-type granite porphyry in West Junggar, Xinjiang, China[J]. Lithos,2014,198 -199(1):172-183.
APA Wei Mao.,Xiaofeng Li.,Guo Wang.,Rong Xiao.,Mou Wang.,...&Feng Yang.(2014).Petrogenesis of the Yangzhuang Nb- and Ta-rich A-type granite porphyry in West Junggar, Xinjiang, China.Lithos,198 -199(1),172-183.
MLA Wei Mao,et al."Petrogenesis of the Yangzhuang Nb- and Ta-rich A-type granite porphyry in West Junggar, Xinjiang, China".Lithos 198 -199.1(2014):172-183.
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