The anatomy of the 750 Ma Bavali shear zone in South India: did the integration of India into East Gondwanaland initiate in the mid-Neoproterozoic?
Author:
Funder
Science and Engineering Research Board, Govt. of India
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s00531-023-02355-w.pdf
Reference203 articles.
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2. Amaldev T, Santosh M, Tang L, Baiju KR, Tsunogae T, Satyanarayanan M (2016) Mesoarchean convergent margin processes and crustal evolution: Petrologic, geochemical and zircon U-Pb and Lu–Hf data from the Mercara Suture Zone, Southern India. Gond Res 37:182–204. https://doi.org/10.1016/j.gr.2016.05.017
3. Anderson DL (1994) Superplume or supercontinents? Geology 22:39–42. https://doi.org/10.1130/0091-7613(1994)022%3C0039:SOS%3E2.3.CO;2
4. Babinski M, Chemale F, Hartman L, van Schmus WR, da Silva LC (1996) Juvenile accretion at 750–700 Ma in Southern Brazil. Geology 24:439‒442. https://doi.org/10.1130/0091-7613(1996)024<0439:JAAMIS>2.3.CO;2s
5. Banerjee A, Sequeira N, Bhattacharya A (2021) Tectonics of the Greater India Proterozoic Fold Belt, with emphasis on the nature of curvature of the belt in West-central India. Earth Sci Rev 221:103758. https://doi.org/10.1016/j.earscirev.2021.103758
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