Tectonic forcing of evolution and Holocene erosion rate of ravines in the Marginal Ganga Plain, India

Author:

Ghosh R.,Srivastava P.,Shukla U.K.,Singh I.,Champati Ray P.K.,Sehgal R.K.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference82 articles.

1. Extensional tectonic activity in the cratonward parts (peripheral bulge) of the Ganga Plain foreland basin, India;Agarwal;Int. J. Earth Sci.,2002

2. Agarwal, R.K., 1977. Structure and tectonics of Indo-Gangetic plains. In: Geophysical Case Histories of India. AEG Seminar, Hyderabad 1, 29–46.

3. The Dynamics of Faulting and Dyke Formation With Applications to Britain;Anderson,1951

4. An Introduction to Optical Dating: The Dating of Quaternary Sediments by the Use of Photon-Stimulated Luminescence;Aitken,1998

5. Controls on morphological variability and role of stream power distribution pattern, Yamuna River, western India;Bawa;Geomorphology,2014

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