Intrusion and upliftment of Mahakoshal rocks between Vindhyan and Gondwana in Narmada Son Lineament, Central India

Author:

Ghosh G. K.,Singh C. L.

Publisher

Springer Science and Business Media LLC

Subject

Geology

Reference46 articles.

1. Acharya, S.K. and Roy, Abhinaba (2000) Tectonothermal history of the central Indian tectonics zone and reactivation of major faults/shear zone. Jour. Geol. Soc. India, v.55(3), pp.239–256.

2. Akhtar, K. (1996) Facies, sedimentation process and environments in the Proterozoic Vindhyan basin, India. In: A. Bhattacharya (Ed.), Recent advances in Vindhyan Geology. Mem. Geol. Soc. India, no.36, pp.127–136.

3. Arora, B.R. (2000) Geomagnetic deep sounding studies in India: tectonics implications. Indian Geological Congress, Special Volume 1, pp.113–122.

4. Arora, B.R., Waghmare, S.Y. and Mahashabde, M.V. (1995) Geomagnetic depth sounding along the Hirapur-Mandla-Bhandara profile, Central India. Mem. Geol. Soc. India, no.31, pp.519–535.

5. Bhattacharjee, S. and Koide, H. (1978) The origin and evaluation of rifts and rift valley structures: A mechanistic interpretation in Tectonic and Geophysics of continental rifts, Eds. I.B. Ramberg and E.R., 11–28, Reidel Publishing Co., Dordrecht Holland.

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