Volume 12 Issue 4
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Manoj K. Pandit, Hitesh Kumar, Wei Wang. Geochemistry and geochronology of A-type basement granitoids in the north-central Aravalli Craton: Implications on Paleoproterozoic geodynamics of NW Indian Block[J]. Geoscience Frontiers, 2021, 12(4): 101084. doi: 10.1016/j.gsf.2020.09.013
Citation: Manoj K. Pandit, Hitesh Kumar, Wei Wang. Geochemistry and geochronology of A-type basement granitoids in the north-central Aravalli Craton: Implications on Paleoproterozoic geodynamics of NW Indian Block[J]. Geoscience Frontiers, 2021, 12(4): 101084. doi: 10.1016/j.gsf.2020.09.013

Geochemistry and geochronology of A-type basement granitoids in the north-central Aravalli Craton: Implications on Paleoproterozoic geodynamics of NW Indian Block

doi: 10.1016/j.gsf.2020.09.013

We would like to thank Erkum Xue for his help in analytical work. We also thank Rajesh Sharma and A.K. Singh for help and support in XRF and ICP-MS analysis of samples. We thank two anonymous reviewers for their useful comments that have helped in improving the paper. We thank Lily Wang and Vinod Samuel for excellent editorial handling of the manuscript. The geochemical plots were prepared with the help of open-access software GCD Kit.

  • Received Date: 2020-05-17
  • Rev Recd Date: 2020-08-25
  • Publish Date: 2021-07-17
  • The basement granite gneisses from the north-central Aravalli Craton in NW India were investigated for geochemistry and geochronology. In a peneplain terrain, the granite gneiss outcrops are scanty and samples were collected mainly from two small hills and several ground-level exposures in the Sakhun-Ladera region. Well-foliated granite gneiss is the dominant lithology that also hosts dark, lenticular enclaves, and is in turn, intruded by mafic dykes. The granite gneiss has silica content ranging from 61.37 wt.% to 68.27 wt.% that marks a slight overlap with the enclaves (54.32 wt.% to 62.17 wt.%). Both groups have a high K2O/Na2O ( ~2 or higher) ratio. Geochemically, the granite gneiss classify as granite-granodiorite, and enclaves as granodiorite-diorite. The In-situ LA-ICP-MS zircon U-Pb geochronology of granite gneiss has yielded a statistically valid 1721 ±9 Ma age that we interpret as the emplacement age for the granitic protolith. Geochemical characteristics of granite gneiss underline fractional crystallization of an I-type melt as the main process, and continuity of trends in enclaves underlines their mutual genetic link. The genetic association is further verified by a consistency in the trace element characteristics and REE patterns. The Nd-isotope signatures define a single grouping for both granite gneiss and enclaves, with εNd(t) values ranging from -6.38 to -6.61, further substantiating a common source. The geochemical tectonic discrimination schemes consistently point toward an extensional setting and A-type characteristics for granite gneiss and enclaves. These are analogous to the coeval (1.72-1.75 Ga), A-type granitoids from the Khetri and Alwar basin in the North Delhi Fold Belt, implying a much larger areal extent for the Paleoproterozoic anorogenic magmatism in the northern segment of the Aravalli Craton. The Paleoproterozoic age for the presumed ‘Archean’ basement in this region offers tacit evidence that the BGC-II is a stratigraphically younger terrane as compared to the Archean age, BGC-I.

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