Detrital mode and geochemical constraints on the provenance, paleoweathering and tectonic setting of the Surma sediments of Chittagong-Tripura fold belt, Tripura, India-Reference-Cited by-同舟云学术

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Detrital mode and geochemical constraints on the provenance, paleoweathering and tectonic setting of the Surma sediments of Chittagong-Tripura fold belt, Tripura, India

Published:2024-06 Issue: Volume:134 Page:103590
ISSN:1474-7065
Container-title:Physics and Chemistry of the Earth, Parts A/B/C
language:en
Short-container-title:Physics and Chemistry of the Earth, Parts A/B/C

Author:

Imchen Watitemsu^ORCID,Saha Omnath

Publisher

Elsevier BV

Reference225 articles.

1. Collisional emplacement history of the Naga‐Andaman ophiolites and the position of the eastern Indian suture;Acharyya;J. Asian Earth Sci.,2007

2. Indo‐Burma Range: a belt of accreted microcontinents, ophiolites and Mesozoic–Paleogene ﬂyschoid sediments;Acharyya;Int. J. Earth Sci.,2015

3. Geology and depositional history of Cenozoic sediments of the Bengal Basin of Bangladesh;Alam;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1989

4. Tide-dominated sedimentation in the upper tertiary succession of the sitapahar anticline, Bangladesh;Alam,1995

5. An overview of the sedimentary geology of the Bengal basin in relation to the regional tectonic framework and basin-fill history;Alam;Sediment. Geol.,2003

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