Precambrian mafic dyke swarms from the central Indian Bastar craton
Author:
Publisher
Taylor & Francis
Link
http://www.crcnetbase.com/doi/pdf/10.1201/NOE0415398992.ch10
Reference42 articles.
1. Mantle composition derived from the chemistry of ultramafic lavas
2. Petrogenetic relationship between Palaeoproterozoic tholeiitic dykes and associated high-Mg noritic dykes, Labrador, Canada
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1. Petrography and Major Oxide Geochemistry of Dolerite Dykes from Kunnam Region Villupuram, Tamil Nadu, Southern India;Advances in Geographical and Environmental Sciences;2024
2. Precise Pb-Pb baddeleyite geochronology, geochemistry, and Sr-Nd isotopic constraints on the 2.36 & 1.88 Ga mafic dykes from the Bastar craton, India: Implications for their petrogenesis in conjunction with the Dharwar mafic dykes;Precambrian Research;2023-08
3. Geochemistry, magma flow characteristics and petrogenesis of Paleoproterozoic NW–NNW trending mafic dykes from central Bastar craton, India;Journal of Earth System Science;2022-12-23
4. Geochronology, whole-rock geochemistry and Sr-Nd isotopes of the Bhanupratappur mafic dyke swarm: Evidence for a common Paleoproterozoic LIP event at 2.37–2.36 Ga in the Bastar and Dharwar cratons;Precambrian Research;2020-09
5. Precambrian mafic dyke swarms in the Singhbhum craton (eastern India) and their links with dyke swarms of the eastern Dharwar craton (southern India);Precambrian Research;2019-08
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