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DOI | 10.1016/j.jseaes.2015.02.017 |
Petrogenesis and tectonic setting of Triassic granitoids in the Qiangtang terrane, central Tibet: Evidence from U-Pb ages, petrochemistry and Sr-Nd-Hf isotopes | |
Li, Guang-Ming; Li, Jin-Xiang; Zhao, Jun-Xing; Qin, Ke-Zhang; Cao, Ming-Jian; Evans, Noreen J. | |
通讯作者 | Li, GM (通讯作者) |
发表日期 | 2015 |
ISSN | 1367-9120 |
EISSN | 1878-5786 |
起始页码 | 443 |
结束页码 | 455 |
卷号 | 105 |
英文摘要 | Triassic granitoids, including the similar to 220 Ma Shuanghu and similar to 210 Ma Rongma granitoids studied here, are widely distributed around the-Longmu-Shuanghu suture and in the Qiangtang terrane, central Tibet. The majority of these granitoids can be classified as high-K calc-alkaline in nature and yield negative Ba and Sr anomalies on primitive mantle-normalized diagrams. In addition, they are: enriched in light rare earth elements (LREE) ((La/Yb)(N) = 1.61-21.79); strongly enriched in large ion lithophile elements (LILE: e.g., Cs, Rb, and K), and depleted in high field strength elements (HFSE: e.g., Nb and Ti). Magma mixing played a role in the genesis of the Shuanghu granodiorites, as indicated by the occurrence of dioritic enclaves and the wide range in zircon Hf compositions (epsilon Hf(t) = -15.0 to -2.5). The I-type Shuanghu granodiorites and S-type Shuanghu and Rongma granites might have been derived from melting of southern Qiangtang crust given the high initial Sr (0.7131-0.7272), low epsilon Nd(t) (-8.9 to -11.1) and zircon epsilon Hf(t) values (-15 to -7.2). The granitoids may have formed during melting of southern Qiangtang crust, heated by upwelling asthenosphere mantle, a result of break-off and delamination of the Paleo-Tethys slab in a collisional setting. (C) 2015 Elsevier Ltd. All rights reserved. |
关键词 | ZIRCON REFERENCE MATERIALNORTHERN TIBETLU-HFMASS-SPECTROMETRYARC MAGMATISMMETAMORPHIC BELTVOLCANIC-ROCKSTRACE-ELEMENTPALEO-TETHYSTH-PB |
英文关键词 | Geochronology; Zircon Hf isotopes; Granitoids; Qiangtang terrane; Tibet |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000355051700029 |
来源期刊 | JOURNAL OF ASIAN EARTH SCIENCES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258548 |
推荐引用方式 GB/T 7714 | Li, Guang-Ming,Li, Jin-Xiang,Zhao, Jun-Xing,et al. Petrogenesis and tectonic setting of Triassic granitoids in the Qiangtang terrane, central Tibet: Evidence from U-Pb ages, petrochemistry and Sr-Nd-Hf isotopes[J]. 中国科学院青藏高原研究所,2015,105. |
APA | Li, Guang-Ming,Li, Jin-Xiang,Zhao, Jun-Xing,Qin, Ke-Zhang,Cao, Ming-Jian,&Evans, Noreen J..(2015).Petrogenesis and tectonic setting of Triassic granitoids in the Qiangtang terrane, central Tibet: Evidence from U-Pb ages, petrochemistry and Sr-Nd-Hf isotopes.JOURNAL OF ASIAN EARTH SCIENCES,105. |
MLA | Li, Guang-Ming,et al."Petrogenesis and tectonic setting of Triassic granitoids in the Qiangtang terrane, central Tibet: Evidence from U-Pb ages, petrochemistry and Sr-Nd-Hf isotopes".JOURNAL OF ASIAN EARTH SCIENCES 105(2015). |
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