Depositional architecture of sub-aqueous part of a tide-dominated delta and its palaeogeographic implications: Laisong Formation (Barail Group), Indo-Myanmar Ranges, western Manipur

Author:

Kumar Pramod,Devi Kshetrimayum Lakshmirani,Chakraborty Partha Pratim,Rajkumar Hemanta Singh

Funder

Research and Development (R&D Grant) Delhi University

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference109 articles.

1. Acharyya S K 1986 Tectono-stratigraphic history of Naga hill ophiolites; Geol. Surv. India Memoir 119 94–103.

2. Acharyya S K 2007 Collisional emplacement history of the Naga–Andaman ophiolites and the position of the eastern Indian suture; J. Asian Earth Sci. 29 229–242.

3. Acharyya S K 2010 Tectonic evolution of Indo-Burma range with special reference to Naga Manipur hills; Geol. Soc. India Memoir 75 25–43.

4. Acharyya S K 2015 Indo Burma range: A belt of accreted microcontinents, ophiolites and Mesozoic–paleogene flyschoid sediments; Int. J. Earth Sci. 104 1235–1251.

5. Acharyya S K, Mitra N D and Nandy D R 1986 Regional geology and tectonic settings of Northeast India and adjoining regions; Geol. Surv. India Memoir 119 6–12.

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