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DOI | 10.1130/B31653.1 |
Petrogenesis of mafic and felsic rocks from the Comei large igneous province, South Tibet: Implications for the initial activity of the Kerguelen plume | |
Zhou Q.; Liu Z.; Lai Y.; Wang G.-C.; Liao Z.; Li Y.-X.; Wu J.-Y.; Wang S.; Qing C.-S. | |
发表日期 | 2018 |
ISSN | 167606 |
起始页码 | 811 |
结束页码 | 824 |
卷号 | 130期号:2021-05-06 |
英文摘要 | The role of the Kerguelen plume in breaking up eastern Gondwana is so far unclear. Recently, the initial magmatic record of the plume has been identified in the Comei igneous province, Tethyan Himalaya. In this contribution, we investigated a group of basaltic intrusions (Juelongpu and Zhaxikang) and felsic lavas (Sangxiu) from the Comei igneous province. Laser ablation-inductively coupled plasma-mass spectrometry zircon U-Pb dating indicates that these mafic and felsic rocks were emplaced in the Early Cretaceous (ca. 140-137 Ma). Probably originating from the Kerguelen plume, the Juelongpu and Zhaxikang mafic rocks are characterized by high incompatible element abundances, high Nb/Y ratios, and oceanic-island basalt- like rare earth element and trace-element patterns. The Sangxiu felsic samples share A-type affinities and were derived by partial melting of crustal rocks. These mafic and felsic rocks represent a magmatic response to the initial activity of the Kerguelen plume. Their ages (ca. 140-137 Ma) are older than the timing of initial breakup of eastern Gondwana (ca. 137-136 Ma), indicating that the plume must have been incubating underneath the supercontinent before the breakup. Recent plate reconstructions coupled with our geochemical and geochronological constraints suggest that the Kerguelen plume head was resident under the Comei area of Greater India. at ca. 140 Ma. Our results, in conjunction with previous studies, support the viewpoint that the Kerguelen plume played an active role in breaking up eastern Gondwana. © 2017 Geological Society of America. |
语种 | 英语 |
来源期刊 | Bulletin of the Geological Society of America
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/185033 |
作者单位 | Chengdu Institute of Geology and Mineral Resources, Chinese Geological Survey, Chengdu, 610081, China; School of Earth Sciences, Gansu Key Laboratory of Mineral Resources in Western China, Lanzhou University, Lanzhou, 730000, China; State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210046, China |
推荐引用方式 GB/T 7714 | Zhou Q.,Liu Z.,Lai Y.,et al. Petrogenesis of mafic and felsic rocks from the Comei large igneous province, South Tibet: Implications for the initial activity of the Kerguelen plume[J],2018,130(2021-05-06). |
APA | Zhou Q..,Liu Z..,Lai Y..,Wang G.-C..,Liao Z..,...&Qing C.-S..(2018).Petrogenesis of mafic and felsic rocks from the Comei large igneous province, South Tibet: Implications for the initial activity of the Kerguelen plume.Bulletin of the Geological Society of America,130(2021-05-06). |
MLA | Zhou Q.,et al."Petrogenesis of mafic and felsic rocks from the Comei large igneous province, South Tibet: Implications for the initial activity of the Kerguelen plume".Bulletin of the Geological Society of America 130.2021-05-06(2018). |
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