Indo-Burma Range: a belt of accreted microcontinents, ophiolites and Mesozoic–Paleogene flyschoid sediments-Reference-Cited by-同舟云学术

Indo-Burma Range: a belt of accreted microcontinents, ophiolites and Mesozoic–Paleogene flyschoid sediments

Published:2015-03-31 Issue:5 Volume:104 Page:1235-1251
ISSN:1437-3254
Container-title:International Journal of Earth Sciences
language:en
Short-container-title:Int J Earth Sci (Geol Rundsch)

Author:

Acharyya S. K.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s00531-015-1154-6.pdf

Reference56 articles.

1. Acharyya SK (1986) Tectono-stratigraphic history of Naga Hills Ophiolites. In: Geology of Nagaland ophiolite. Geol Surv India Mem 119:94–103

2. Acharyya SK (1996) Accretion of Indo-Australian Gondwanic blocks along peri-Indian collision margins. In: Gondwana 9, International Gondwana Symposium, Hyderabad, 1994, India, Oxford IBH, New Delhi, pp 1029–1049

3. Acharyya SK (1998) Break-up of the Greater Indo-Australian continent and accretion of blocks framing South and East Asia. Geodynamics 26:149–170

4. Acharyya SK (2007a) Collisional emplacement history of the Naga-Andaman ophiolites and the position of the eastern Indian suture. J Asian Earth Sci 29:229–242

5. Acharyya SK (2007b) Evolution of the Himalayan Paleogene foreland basin, influence of its litho-packet on the formation of thrust-related domes and windows in the Eastern Himalayas—a review. J Asian Earth Sci 31:1–17

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