| Autor: |
Kaila, K.L., Murty, P.R.K., Mall, D.M. |
| Zdroj: |
Tectonophysics; January 1989, Vol. 162 Issue: 3 p277-289, 13p |
| Abstrakt: |
The evolution of the Vindhyan basin has been studied from deep seismic soundings. Block tectonics appear to be active throughout the geological history in this region. The crust is divided into four major blocks by deep faults at Narsinghgarh, Katangi and Jabalpur. The crustal block between Narsinghgarh and Katangi forms a graben in the crystalline basement, giving rise to the great Vindhyan basin in which Precambrian Vindhyan sediments of about 5.5 km thickness are deposited. The crustal block between Katangi and Jabalpur is a horst block which represents the Narmada-Son lineament. |
| Databáze: |
Supplemental Index |
| Externí odkaz: |
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