Paleogene evolution of the Burmese forearc basin and implications for the history of India-Asia convergence

Author:

Licht Alexis1,Dupont-Nivet Guillaume234,Win Zaw5,Swe Hnin Hnin6,Kaythi Myat6,Roperch Pierrick2,Ugrai Tamas1,Littell Virginia1,Park Diana1,Westerweel Jan2,Jones Dominic1,Poblete Fernando27,Aung Day Wa6,Huang Huasheng8,Hoorn Carina8,Sein Kyaing9

Affiliation:

1. Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195, USA

2. Géosciences Rennes, UMR CNRS 6118, Université de Rennes, 35042 Rennes Cedex, France

3. Potsdam University, Institute of Earth and Environmental Science, 14476 Potsdam, Germany

4. Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Beijing, China

5. Geology Department, Shwe Bo University, Sagaing Region, Myanmar

6. Geology Department, University of Yangon, Pyay Road, Yangon, Myanmar

7. Instituto de Ciencias de la Ingeniería, Universidad de O’Higgins, Rancagua, Chile

8. Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, 1098 XH Amsterdam, The Netherlands

9. Myanmar Geosciences Society, Yangon, Myanmar

Publisher

Geological Society of America

Subject

Geology

Reference129 articles.

1. Collisional emplacement history of the Naga-Andaman ophiolites and the position of the eastern Indian suture;Acharyya;Journal of Asian Earth Sciences,2007

2. Indo-Burma Range: a belt of accreted microcontinents, ophiolites and Mesozoic–Paleogene flyschoid sediments;Acharyya;International Journal of Earth Sciences,2015

3. First myliobatiform teeth (Elasmobranchii, Neoselachii) from the pondaung formation (late middle Eocene) of central Myanmar;Adnet;Neues Jahrbuch für Geologie und Palaontologie, Abhandlungen,2008

4. When and where did India and Asia collide?;Aitchison;Journal of Geophysical Research. Solid Earth,2007

5. Structure and evolution of the Himalaya–Tibet orogenic belt;Allègre;Nature,1984

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