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Petrology and geochemistry of postcollisional volcanic rocks from the Tibetan plateau: Implications for lithosphere heterogeneity and collision-induced asthenospheric mantle flow

By
Xuanxue Mo
Xuanxue Mo
State Key Laboratory of Geological Processes and Mineral Resources and School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China
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Zhidan Zhao
Zhidan Zhao
State Key Laboratory of Geological Processes and Mineral Resources and School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China
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Jinfu Deng
Jinfu Deng
State Key Laboratory of Geological Processes and Mineral Resources and School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China
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Martin Flower
Martin Flower
Department of Earth and Environmental Sciences, University of Illinois at Chicago (m/c 186), 845 West Taylor Street, Chicago, Illinois 60607-7059, USA
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Xuehui Yu
Xuehui Yu
State Key Laboratory of Geological Processes and Mineral Resources and Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology, China University of Geosciences, Ministry of Education of China, Beijing 100083, China
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Zhaohua Luo
Zhaohua Luo
State Key Laboratory of Geological Processes and Mineral Resources and Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology, China University of Geosciences, Ministry of Education of China, Beijing 100083, China
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Youguo Li
Youguo Li
Department of Geology, Chengdu University of Science and Technology, Chengdu 610059, China
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Su Zhou
Su Zhou
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
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Guochen Dong
Guochen Dong
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
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Dicheng Zhu
Dicheng Zhu
Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China
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Liangliang Wang
Liangliang Wang
School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China
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Published:
January 01, 2006

This article summarizes the geological setting, spatial-temporal distribution, and major-element, trace-element, and Nd-Sr-Pb isotopic compositional variation of rocks representative of Tibetan postcollisional magmatic activity. The implications of petrogenesis and spatial-temporal distribution are discussed in relation to lithospheric mantle heterogeneity and a possible role for collision-induced asthenospheric mantle flow. Rocks indicative of postcollisional volcanism are widely distributed across the terranes making up the Tibetan plateau. Three stages of activity are recognized (ca. 45–25, 25–5, and 5–0 Ma), mostly conforming to potassic to ultrapotassic shoshonitic and high-potassium calc-alkaline types. These show strong relative enrichments in large-ion lithophile elements (LILE), U, Th, and light rare earth elements (LREE); depletions in high field strength elements (HFSE) and heavy rare earth elements (HREE)—with (La/Yb)N ratios ranging from 4.3 to 699, mainly 40–50; ∑REE and abundances of 50–2560 ppm, mainly 300–500 ppm—in most cases lacking significant negative Eu anomalies. However, the element distributions for kamafugite and carbonatite show ocean island basalt–like nondepleted or even slightly enriched HFSE patterns. The plots of ϵNd versus 87Sr/86Sr define a mixing array between Neo-Tethyan mid-ocean ridge basalts (MORB) and High Himalayan crustal compositions, with ϵNd(t) varying from +5.95 to −17.42 and 87Sr/86Sr (i) 0.702059 to 0.746320. The range of Nd and Sr isotopic compositions in the northern parts of the plateau, Sanjiang, and west Qinling is relatively small compared to that from Gangdese to the south, where 87Sr/86Sr ratios range from 0.703785 to 0.746320 and 143Nd/144Nd from 0.511737 to 512710. The variation of Pb isotopic ratios is somewhat less, with 206Pb/204Pb ranging from 18.149 to 19.345, 207Pb/204Pb from 15.476 to 15.803, and 208Pb/204Pb from 37.613 to 40.168. In general, magmatic isotopic compositions indicate the regional-scale presence of DUPAL-like mantle, reflecting additions of the “enriched mantle” components (EM1, EM2) to an ambient MORB-HIMU (high μ, i.e., high U/Pb mantle) asthenospheric hybrid.

The observed geochemical, isotopic, and mineral phase compositional variations of primitive magmatic products and their entrained mantle xenoliths clearly suggest LILE-enriched and HFSE-depleted phlogopite/amphibole–bearing mantle wedge sources contaminated by (presumably subduction-related) hydrous fluids or smallfraction H2O-CO2–rich melts. Tibetan lithospheric mantle appears to reflect the presence of and interaction between at least three compositional end-members. The overall spatial-temporal pattern of Tibetan collisional and postcollisional activity is consistent with the hypothesis that the Neo-Tethyan asthenospheric mantle was laterally displaced along discrete northeast- and southwestward flow channels in response to the IndiaAsia collision.

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GSA Special Papers

Postcollisional Tectonics and Magmatism in the Mediterranean Region and Asia

Yildirim Dilek
Yildirim Dilek
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Spyros Pavlides
Spyros Pavlides
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Geological Society of America
Volume
409
ISBN print:
9780813724096
Publication date:
January 01, 2006

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