中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geochronology and petrogenesis of the TTG gneisses and granitoids from the Central Bundelkhand granite-greenstone terrane, Bundelkhand Craton, India: Implications for Archean crustal evolution and cratonization

文献类型:期刊论文

作者Singh, Pradip K.2,3,4,5; Verma, Sanjeet K.2; Singh, Vinod K.6; Moreno, Juan A.7; Oliveira, Elson P.3; Li, Xian-Hua5; Malviya, Vivek P.1; Prakash, Divya4
刊名PRECAMBRIAN RESEARCH
出版日期2021-07-01
卷号359页码:23
关键词Bundelkhand Craton Granite-greenstone terrane Zircon dating Lu-Hf isotopes Sm-Nd isotopes Juvenile and reworked crusts
ISSN号0301-9268
DOI10.1016/j.precamres.2021.106210
英文摘要In this contribution we present field relations, U-Pb zircon geochronology, in-situ Lu-Hf isotopes, bulk-rock SmNd isotopes and geochemistry of the tonalite-trondhjemite-granodiorite (TTG) gneiss, sanukitoid and anatectic granites from the Central Bundelkhand granite-greenstone terrane (CBGGT). The present study provides a comprehensive insight into the crust-mantle evolution, reworking, and cratonization of the Bundelkhand Craton (BC) during the Archean Eon. We report two discrete episodes of Neoarchean TTG magmatism at similar to 2.71 and similar to 2.68 Ga from the BC for the first time. Additionally, we identify a TTG gneiss that is significantly older (similar to 3.34 Ga) than thus far assumed in the eastern part of the area. Furthermore, zircon U-Pb ages of the sanukitoids and the anatectic granites suggest synchronous emplacement at 2.58-2.50 Ga. Zircon of Paleoarchean TTG, Neoarchean TTG, sanukitoid, and anatectic granites show epsilon Hf-(t) values in the following ranges: +1.7 to 0.9, +4.1 to -10.7, -3.6 to -6.2, and -5.9 to -7.8, respectively, which are indicative of significant crustal reworking. Neoarchean TTG gneiss shows epsilon Nd-(t) and epsilon Hf-(t) value of + 4.5 and + 10.0 to -6.8, respectively, indicating a juvenile crustal source and probably formed by the partial melting of deep-seated mafic crust in the garnet stability field. Neoarchean TTGs formed in arc creation/collision to the Paleoarchean nucleus of the BC. The amalgamation of diverse micro-blocks occurred by the arc-continent collision and probable breakoff of the descending slab between crustal blocks of the BC during Neoarchean. This event generated anatectic granites by intense partial melting of the existing crust, which resulted as closing of subduction and marked as final stabilization and cratonization of the BC. This event also shows evidence that the BC did not amalgamate until similar to 2.50 Ga.
WOS关键词ZIRCON U-PB ; CONTINENTAL-CRUST ; ISOTOPE SYSTEMATICS ; PLATE-TECTONICS ; NORTHERN INDIA ; DHARWAR CRATON ; GEOCHEMISTRY ; CONSTRAINTS ; COMPLEX ; ROCKS
资助项目National Council of Science and Technology (CONACYT), Mexico[612752] ; IPICYT ; Sao Paulo Research Foundation (FAPESP)[2012/07243-3] ; Sao Paulo Research Foundation (FAPESP)[2012/15824-6] ; Newton Advance Fellowship award-The Royal Society, UK[NA160116] ; IGGCAS[2019PR02] ; NSFC[41890831] ; Department of Science and Technology (DST), Government of India[INT/RUS/RFBR/P-279]
WOS研究方向Geology
语种英语
WOS记录号WOS:000652106800021
出版者ELSEVIER
资助机构National Council of Science and Technology (CONACYT), Mexico ; National Council of Science and Technology (CONACYT), Mexico ; IPICYT ; IPICYT ; Sao Paulo Research Foundation (FAPESP) ; Sao Paulo Research Foundation (FAPESP) ; Newton Advance Fellowship award-The Royal Society, UK ; Newton Advance Fellowship award-The Royal Society, UK ; IGGCAS ; IGGCAS ; NSFC ; NSFC ; Department of Science and Technology (DST), Government of India ; Department of Science and Technology (DST), Government of India ; National Council of Science and Technology (CONACYT), Mexico ; National Council of Science and Technology (CONACYT), Mexico ; IPICYT ; IPICYT ; Sao Paulo Research Foundation (FAPESP) ; Sao Paulo Research Foundation (FAPESP) ; Newton Advance Fellowship award-The Royal Society, UK ; Newton Advance Fellowship award-The Royal Society, UK ; IGGCAS ; IGGCAS ; NSFC ; NSFC ; Department of Science and Technology (DST), Government of India ; Department of Science and Technology (DST), Government of India ; National Council of Science and Technology (CONACYT), Mexico ; National Council of Science and Technology (CONACYT), Mexico ; IPICYT ; IPICYT ; Sao Paulo Research Foundation (FAPESP) ; Sao Paulo Research Foundation (FAPESP) ; Newton Advance Fellowship award-The Royal Society, UK ; Newton Advance Fellowship award-The Royal Society, UK ; IGGCAS ; IGGCAS ; NSFC ; NSFC ; Department of Science and Technology (DST), Government of India ; Department of Science and Technology (DST), Government of India ; National Council of Science and Technology (CONACYT), Mexico ; National Council of Science and Technology (CONACYT), Mexico ; IPICYT ; IPICYT ; Sao Paulo Research Foundation (FAPESP) ; Sao Paulo Research Foundation (FAPESP) ; Newton Advance Fellowship award-The Royal Society, UK ; Newton Advance Fellowship award-The Royal Society, UK ; IGGCAS ; IGGCAS ; NSFC ; NSFC ; Department of Science and Technology (DST), Government of India ; Department of Science and Technology (DST), Government of India
源URL[http://ir.iggcas.ac.cn/handle/132A11/102034]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Singh, Pradip K.; Verma, Sanjeet K.
作者单位1.24E Mayur Residency Ext, Lucknow 226015, Uttar Pradesh, India
2.Inst Potosino Invest Cient & Tecnol IPICYT, Div Geociencias Aplicadas, Camino Presa San Jose 2055, San Luis Potosi, San Luis Potosi, Mexico
3.Univ Campinas UNICAMP, Inst Geosci, Dept Geol & Nat Resources, POB 6152, BR-13083970 Campinas, SP, Brazil
4.Banaras Hindu Univ BHU, Ctr Adv Study, Inst Sci, Dept Geol, Varanasi 221005, Uttar Pradesh, India
5.Chinese Acad Sci IGG CAS, Inst Geol & Geophys, State Key Lab Lithospher Evolut, 19 Beitucheng West Rd, Beijing 100029, Peoples R China
6.Bundelkhand Univ, Inst Earth Sci, Dept Geol, Jhansi, Uttar Pradesh, India
7.CICTERRA CONICET UNC, Av Velez Sarsfield 1611,X5016CGA, Cordoba, Argentina
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GB/T 7714
Singh, Pradip K.,Verma, Sanjeet K.,Singh, Vinod K.,et al. Geochronology and petrogenesis of the TTG gneisses and granitoids from the Central Bundelkhand granite-greenstone terrane, Bundelkhand Craton, India: Implications for Archean crustal evolution and cratonization[J]. PRECAMBRIAN RESEARCH,2021,359:23.
APA Singh, Pradip K..,Verma, Sanjeet K..,Singh, Vinod K..,Moreno, Juan A..,Oliveira, Elson P..,...&Prakash, Divya.(2021).Geochronology and petrogenesis of the TTG gneisses and granitoids from the Central Bundelkhand granite-greenstone terrane, Bundelkhand Craton, India: Implications for Archean crustal evolution and cratonization.PRECAMBRIAN RESEARCH,359,23.
MLA Singh, Pradip K.,et al."Geochronology and petrogenesis of the TTG gneisses and granitoids from the Central Bundelkhand granite-greenstone terrane, Bundelkhand Craton, India: Implications for Archean crustal evolution and cratonization".PRECAMBRIAN RESEARCH 359(2021):23.

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来源:地质与地球物理研究所

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