Quaternary Geomorphology in India by Balai Chandra Das Sandipan Ghosh & Aznarul Islam

Author:Balai Chandra Das, Sandipan Ghosh & Aznarul Islam
Language: eng
Format: epub
Publisher: Springer International Publishing, Cham

Fig. 5.7 Basement configuration and subsurface structure has been delineated through integrated interpretation of travel-time inversion of wide-angle seismic sounding reflection data and gravity data. a, In particular, profile CD shows north–south depression in Bouguer gravity values, where maximum depression has been observed over the interfluve of Ajay and Damodar Rivers (lower part); b and profile AB shows variation in gravity value and basement depth with successive formation and different fault lines (Fn): F1 = Mednipur–Farraka Fault or Basin -Margin Fault, F2 = Pingla Fault, F3 = Garhmayna–Khandaghosh Fault, F4 = Damodar Fault and F5 = Memari–Debagram Fault.

Source Modified after Choudhury and Datta (1973), Verma and Mukhopadhyay (1977), Reddy et al. (1993), Murty et al. (2008), Rajasekhar and Mishra (2008), Roy et al. (2010), Banerjee et al. (2013)

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