Geochemistry, Geochronology, Sr-Nd Isotopic Compositions of Jiang Tso Ophiolite in the Middle Segment of the Bangong- Nujiang Suture Zone and Their Geological Significance
The Jiang Tso ophiolite, situated in the middle segment of the Bangong- Nujiang Suture Zone, is a part of the easternmost Qieli Lake ophiolite subzone and is close to the south of Pung Lake ophiolite. The rock association of Jiang Tso ophiolite is relatively complete and is mainly composed of metamo...
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Published in | Acta geologica Sinica (Beijing) Vol. 89; no. 2; pp. 389 - 401 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Richmond
Blackwell Publishing Ltd
01.04.2015
Wiley Subscription Services, Inc Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, Guangzhou 510006, Guangdong, China%Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China%School of Earth Science and Geological Engineering, Sun Yat-sen University, Guangzhou 510275,Guangdong, China School of Marine sciences, Sun Yat-Sen University, Guangzhou 510006, Guangdong, China Key Laboratory of Offshore Oil Exploration and Development, Guangdong University, Guangzhou 510006, Guangdong, China |
Edition | English ed. |
Subjects | |
Online Access | Get full text |
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Summary: | The Jiang Tso ophiolite, situated in the middle segment of the Bangong- Nujiang Suture Zone, is a part of the easternmost Qieli Lake ophiolite subzone and is close to the south of Pung Lake ophiolite. The rock association of Jiang Tso ophiolite is relatively complete and is mainly composed of metamorphic peridotite, gabbro and diabase. Comparing with N-MORB, the ophiolite is high in Mg and low in Ti, K, Na, P, and is depleted in Nb, Ta, Hf, Th and enriched in Rb, Sr and Ba. Geochemical characteristics of the Jiang Tso ophiolite indicate it is of a supra-subduction zone type formed in the spreading ridge of back arc basin. The SHRIMP U-Pb dating of zircons from the gabbro yielded a weighted average age of 188.1±4.1 Ma (MSWD=1.4), indicating the Jiang Tso ophiolite was formed in the late stage of early Jurassic. The Sr, Nd isotopic compositions show that the Tethyan mantle domain is the depleted mantle (DM), with enriched mantle domain II (EMII). They have the same Sr, Nd isotopic composition with the India Ocean MORB type. |
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Bibliography: | The Jiang Tso ophiolite, situated in the middle segment of the Bangong- Nujiang Suture Zone, is a part of the easternmost Qieli Lake ophiolite subzone and is close to the south of Pung Lake ophiolite. The rock association of Jiang Tso ophiolite is relatively complete and is mainly composed of metamorphic peridotite, gabbro and diabase. Comparing with N-MORB, the ophiolite is high in Mg and low in Ti, K, Na, P, and is depleted in Nb, Ta, Hf, Th and enriched in Rb, Sr and Ba. Geochemical characteristics of the Jiang Tso ophiolite indicate it is of a supra-subduction zone type formed in the spreading ridge of back arc basin. The SHRIMP U-Pb dating of zircons from the gabbro yielded a weighted average age of 188.1±4.1 Ma (MSWD=1.4), indicating the Jiang Tso ophiolite was formed in the late stage of early Jurassic. The Sr, Nd isotopic compositions show that the Tethyan mantle domain is the depleted mantle (DM), with enriched mantle domain II (EMII). They have the same Sr, Nd isotopic composition with the India Ocean MORB type. geochemistry, SHRIMP U-Pb dating, Sr-Nd isotopes, tectonic environment, Tibet 11-2001/P HUANG Qiangtai, LI Jianfeng, CAI Zhourong, XIA Lianze, YUAN Yajuan, LIU Huichuan and XIA Bin(1 School of Marine sciences, Sun Yat-Sen University, Guangzhou 510006, Guangdong, China;2 Key Laboratory of Offshore Oil Exploration andDevelopment, Guangdong University, Guangzhou 510006, Guangdong, China;3 Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, Guangzhou 510006, Guangdong, China;4 Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China;5 School of Earth Science and Geological Engineering, Sun Yat-sen University, Guangzhou 510275, Guangdong, China) istex:20F52901A93B62E7D2FAD53ECFC31DCEB0D695FC ArticleID:ACGS12437 ark:/67375/WNG-JVRH2D9B-Q huangqiangtai@163.com About the first author phone: 020‐39332256, 18922759368. HUANG Qiangtai, male; born in 1986 in Weifang city, Shandong Province; master; postdoctor of School of Marine Sciences, Sun Yat‐sen University; He is now interested in the study on tectonic evolution of Tethyan. E‐mail ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1000-9515 1755-6724 |
DOI: | 10.1111/1755-6724.12437 |