Tectonic Evolution of the Western Margin of the Burma Microplate Based on New Fossil and Radiometric Age Constraints-Reference-Cited by-同舟云学术

Tectonic Evolution of the Western Margin of the Burma Microplate Based on New Fossil and Radiometric Age Constraints

Published:2019-05 Issue:5 Volume:38 Page:1718-1741
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Aitchison Jonathan C.¹^ORCID,Ao Aliba²³^ORCID,Bhowmik Santanu²^ORCID,Clarke Geoffrey L.⁴^ORCID,Ireland Trevor R.⁵^ORCID,Kachovich Sarah¹^ORCID,Lokho Kapesa³^ORCID,Stojanovic Denis¹^ORCID,Roeder Tara⁴,Truscott Naomi⁴,Zhen Yan⁶^ORCID,Zhou Renjie¹^ORCID

Affiliation:

1. School of Earth and Environmental SciencesUniversity of Queensland St Lucia Queensland Australia

2. Department of Geology and GeophysicsIndian Institute of Technology Kharagpur India

3. Wadia Institute of Himalayan Geology Dehra Dun India

4. School of GeosciencesUniversity of Sydney Sydney New South Wales Australia

5. Research School of Earth SciencesAustralian National University Canberra ACT Australia

6. Institute of GeologyChinese Academy of Geological Sciences Beijing China

Funder

Australia-India Strategic Research Fund

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005049

Reference127 articles.

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2. Collisional emplacement history of the Naga-Andaman ophiolites and the position of the eastern Indian suture

3. Tectonic evolution of Indo‐Burma range with special reference to Naga‐Manipur Hills;Acharyya S. K.;Memoir Geological Society India,2010

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

5. Tectono‐stratigraphy and emplacement history of the ophiolite assemblage from the Naga Hills and Andaman island‐arc, India;Acharyya S. K.;Journal Geological Society of India,1989

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