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Chinese Academy of Sciences Institutional Repositories Grid
Geochemistry of Late Palaeoproterozoic (1.69 Ga) A-type Mayong granitoids in Shillong Plateau, north-east India: Implication for anorogenic magmatism during Columbia Supercontinent cycle

文献类型:期刊论文

作者Doley, Dimple2; Bhagabaty, Balen2; Sarma, Gautam2; Singh, Athokapm Krishnakanta3; Zou, Xinyu1
刊名GEOLOGICAL JOURNAL
出版日期2021-10-26
页码19
关键词geochemistry granitoids Mayong north-east India Palaeoproterozoic Shillong Plateau U-Pb ages
ISSN号0072-1050
DOI10.1002/gj.4303
英文摘要The Late Palaeoproterozoic Mayong granitoids of Assam constitute an important component of the continental crust and the Basement Gneissic Complex in the northern extension of the Shillong Plateau, north-east India. The basement rocks of Shillong Plateau are considered as a continuation of the Central Indian Tectonic Zone. In this study, emphasis is given on the new zircon U-Pb age, Hf isotopic composition, and the tectonic implication of Late Palaeoproterozoic Mayong granitoids. The Mayong granitoids are essentially composed of quartz-K-feldspar-plagioclase-biotite-hornblende as major minerals and titanite-zircon-allanite-bastnaesite-apatite-ilmenite as the accessory mineral phase. They show typical geochemical characteristics of A-type granites, such as high silica (average 71.86 wt%), alkalies (average 8.01 wt%), Rb, Zr, Nb, Ga, and rare earth elements (except Eu); high FeOt/MgO and Ga/Al ratios, and low CaO, MgO, Ba, Sr, P, Eu, and Ti concentrations. Laser ablation inductively coupled plasma mass spectrometry zircon U-Pb dating indicates that they were emplaced at similar to 1,687 +/- 35 Ma during the large-scale magmatism of Late Palaeoproterozoic to Early Mesoproterozoic periods. Their zircon Hf model (T-DM2) ages (1,833-2,257 Ma) in conjunction with trace elemental characteristics suggest that they were generated by the reworking/recycling of Early Palaeoproterozoic crust in an intraplate extensional tectonic environment. Thus, we conclude that these A-type Late Palaeoproterozoic Mayong granitoids of the Shillong Plateau probably have a close genetic linkage with the magmatic event of the Columbia Supercontinent cycle during 1,687 +/- 35 Ma.
WOS关键词U-PB ISOTOPE ; PALEO-MESOPROTEROZOIC SUPERCONTINENT ; CHINA CRATON IMPLICATIONS ; ZIRCON LU-HF ; TECTONIC ZONE ; MEGHALAYA PLATEAU ; ARAVALLI OROGEN ; MAHAKOSHAL BELT ; KARBI HILLS ; NW INDIA
资助项目University Grant Commission
WOS研究方向Geology
语种英语
WOS记录号WOS:000711228600001
出版者WILEY
资助机构University Grant Commission ; University Grant Commission ; University Grant Commission ; University Grant Commission ; University Grant Commission ; University Grant Commission ; University Grant Commission ; University Grant Commission
源URL[http://ir.iggcas.ac.cn/handle/132A11/103006]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Bhagabaty, Balen
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Gauhati Univ, Dept Geol Sci, Gauhati 781014, Assam, India
3.Wadia Inst Himalayan Geol, ICP MS Lab, Petrol & Geochem Grp, Dehra Dun 248001, Uttarakhand, India
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GB/T 7714
Doley, Dimple,Bhagabaty, Balen,Sarma, Gautam,et al. Geochemistry of Late Palaeoproterozoic (1.69 Ga) A-type Mayong granitoids in Shillong Plateau, north-east India: Implication for anorogenic magmatism during Columbia Supercontinent cycle[J]. GEOLOGICAL JOURNAL,2021:19.
APA Doley, Dimple,Bhagabaty, Balen,Sarma, Gautam,Singh, Athokapm Krishnakanta,&Zou, Xinyu.(2021).Geochemistry of Late Palaeoproterozoic (1.69 Ga) A-type Mayong granitoids in Shillong Plateau, north-east India: Implication for anorogenic magmatism during Columbia Supercontinent cycle.GEOLOGICAL JOURNAL,19.
MLA Doley, Dimple,et al."Geochemistry of Late Palaeoproterozoic (1.69 Ga) A-type Mayong granitoids in Shillong Plateau, north-east India: Implication for anorogenic magmatism during Columbia Supercontinent cycle".GEOLOGICAL JOURNAL (2021):19.

入库方式: OAI收割

来源:地质与地球物理研究所

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