A Late Cretaceous (ca. 90 Ma) kimberlite event in southern India: Implication for sub-continental lithospheric mantle evolution and diamond exploration
Rao, N. V. Chalapathi1; Dongre, A.2; Wu, Fu-Yuan3; Lehmann, B.4
刊名GONDWANA RESEARCH
2016-07-01
卷号35页码:378-389
关键词Kimberlite Cretaceous Diamond Marion hot-spot Madagascar India
DOI10.1016/j.gr.2015.06.006
文献子类Article
英文摘要We report groundmass perovskite U-Pb (SIMS) ages, perovskite Nd isotopic (LA-ICPMS) composition and bulk rock geochemical data of the Timmasamudram diamondiferous kimberlite cluster, Wajrakarur kimberlite field, in the Eastern Dharwar craton of southern India. The kimberlite pipes gave similar Mesoproterozoic ages of 1086 +/- 19 Ma (TK-1, microcrystic variant) and 1119 +/- 12 Ma (TK-3). However, a perovskite population sampled from the macrocrystic variant of TK-1 gave a much younger Late Cretaceous age of ca. 90 Ma. This macrocrystic kimberlite phase intrudes the Mesoproterozoic microcrystic phase and has a distinct bulk-rock geochemistry. The Nd-isotope composition of the similar to 1100 Ma perovskites in the cluster show depleted epsilon(Nd(T)) values of 2.1 +/- 0.6 to 6.7 +/- 0.3 whereas the similar to 90 Ma perovskites have enriched epsilon(Nd(T)) values of - 63 +/- 1.3. The depleted mantle (DM) model age of the Cretaceous perovskites is 12 Ga, whereas the DM model age of the Proterozoic perovskites is 1.2 to 1.5 Ga. Bulk-rock incompatible trace element ratios (La/Sm, Gd/Lu, La/Nb and Th/Nb) of all Timmasamudram kimberlites show strong affinity with those from the Cretaceous Group II kimberlites from the Bastar craton (India) and Kaapvaal craton (southern Africa). As the Late Cretaceous age of the younger perovskites from the TK-1 kimberlite is indistinguishable from that of the Marion hotspot-linked extrusive and intrusive igneous rocks from Madagascar and India, we infer that all may be part of a single Madagascar Large Igneous Province. Our finding constitutes the first report of Cretaceous kimberlite activity from southern India and has significant implications for its sub-continental lithospheric mantle evolution and diamond exploration programs. (C) 2015 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
WOS关键词PB AGE-DETERMINATION ; SITU U-PB ; STATIONARY MARION HOTSPOT ; LARGE IGNEOUS PROVINCES ; EASTERN DHARWAR CRATON ; ND ISOTOPIC ANALYSIS ; BREAK-UP ; FLOOD BASALTS ; MESOPROTEROZOIC KIMBERLITES ; PALEOMAGNETIC EVIDENCE
WOS研究方向Geology
语种英语
WOS记录号WOS:000384702400025
资助机构Department of Science and Technology, New Delhi(SR/FTP/ES-175/2010) ; Department of Science and Technology, New Delhi(SR/FTP/ES-175/2010) ; Alexander von Humboldt Foundation, Germany ; Alexander von Humboldt Foundation, Germany ; Department of Science and Technology, New Delhi(SR/FTP/ES-175/2010) ; Department of Science and Technology, New Delhi(SR/FTP/ES-175/2010) ; Alexander von Humboldt Foundation, Germany ; Alexander von Humboldt Foundation, Germany
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/53312]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位1.Banaras Hindu Univ, Dept Geol, Ctr Adv Study, Varanasi 221005, Uttar Pradesh, India
2.Univ Johannesburg, Dept Geol, ZA-2006 Auckland Pk, South Africa
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
4.Tech Univ Clausthal, Mineral Resources, D-38678 Clausthal Zellerfeld, Germany
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Rao, N. V. Chalapathi,Dongre, A.,Wu, Fu-Yuan,et al. A Late Cretaceous (ca. 90 Ma) kimberlite event in southern India: Implication for sub-continental lithospheric mantle evolution and diamond exploration[J]. GONDWANA RESEARCH,2016,35:378-389.
APA Rao, N. V. Chalapathi,Dongre, A.,Wu, Fu-Yuan,&Lehmann, B..(2016).A Late Cretaceous (ca. 90 Ma) kimberlite event in southern India: Implication for sub-continental lithospheric mantle evolution and diamond exploration.GONDWANA RESEARCH,35,378-389.
MLA Rao, N. V. Chalapathi,et al."A Late Cretaceous (ca. 90 Ma) kimberlite event in southern India: Implication for sub-continental lithospheric mantle evolution and diamond exploration".GONDWANA RESEARCH 35(2016):378-389.
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