Assessment of the tectonically induced Quaternary landforms and active deformation in the area between Main Boundary Thrust and Himalayan Frontal Thrust, south of the Siang Antiform, Arunachal Himalaya, India

Author:

Luirei Khayingshing1,Kothyari Girish Ch.2,Dumka Rakesh K.2,Bhakuni Surendra S.3

Affiliation:

1. Wadia Institute of Himalayan Geology Dehradun India

2. Active Fault Research Group Institute of Seismological Research Gandhinagar India

3. Talli Bamori Kham Haldwani India

Publisher

Wiley

Subject

Geology

Reference127 articles.

1. Biostratigraphic studies of the continental and marine Gondwana and new light on the pre‐Gondwana rocks of Arunachal Himalaya;Acharya S. K.;Indian Minerals,1974

2. Geological framework of the eastern Himalayas in parts of Kameng, Subansiri, Siang districts, Arunachal Pradesh;Acharya S. K.;Miscellaneous Publications of the Geological Survey of India,1983

3. Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: Implications for seismic hazard

4. The Somme valley terrace system (northern France); a model of river response to Quaternary climatic variations since 800,000 bp

5. Study of crustal movements across Shali Thrust in the area of Shanan (Joginder Nagar) in Himachal Pradesh

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