MD 116 / ANDAMAN

Type Oceanographic cruise
Ship Marion Dufresne
Ship owner TAAF
Dates 29/04/2000 - 01/06/2000
Chief scientist(s) CHAMOT-ROOKE Nicolas ORCID

LABORATOIRE DE GEOLOGIE - ENS

24, rue L'homond

75231 PARIS CEDEX 05

+33(0)1 44.32.22.11

https://www.geologie.ens.fr/

DOI 10.17600/200030
Objective The ANDAMAN cruise aimed to better understand the mechanisms of the opening of the Andaman margin basin. It is located on the eastern flank of the Indian-Eurasian collision along the so-called East-Indian "rail". During the Tertiary, the Andaman-Nicobar complex recorded the progressive migration towards northern India. Three geological objects related to the rapid convergence of the Indian plate towards Eurasia were studied through the ANDAMAN cruise: the active axis of the Andaman Sea and the relationship with the strike-slip fault of Sagaing in Myanmar, the West Burmese scarp associated with the highly oblique subduction of the Indian plate and the Tertiary deformations of the 90°E Ridge

Data managed by SISMER

Bibliography

Publications

Stevens Duncan E., McNeill Lisa C., Henstock Timothy J., Delescluse Matthias, Chamot-Rooke Nicolas, Bull Jonathan M. (2020). A complete structural model and kinematic history for distributed deformation in the Wharton Basin. Earth And Planetary Science Letters, 538, 116218 (12p.). Publisher's official version : https://doi.org/10.1016/j.epsl.2020.116218 , Open Access version : https://archimer.ifremer.fr/doc/00617/72936/


McNeill Lc, Dugan B, Petronotis Ke, Backman J, Bourlange S, Chemale F, Chen W, Colson Ta, Frederik Mcg, Guerin G, Hamahashi M, Henstock T, House Bm, Hupers A, Jeppson Tn, Kachovich S, Kenigsberg Ar, Kuranaga M, Kutterolf S, Milliken Kl, Mitchison Fl, Mukoyoshi H, Nair N, Owari S, Pickering Kt, Pouderoux Hfa, Yehua S, Song I, Torres Me, Vannucchi P, Vrolijk Pj, Yang T, Zhao X, And The Expedition 362 Scientists (2017). Expedition 362 methods. Proceedings of the International Ocean Discovery Program, 362, 1-59. https://doi.org/10.14379/iodp.proc.362.102.2017


Morley C. K., Alvey A. (2015). Is spreading prolonged, episodic or incipient in the Andaman Sea? Evidence from deepwater sedimentation. Journal Of Asian Earth Sciences, 98, 446-456. https://doi.org/10.1016/j.jseaes.2014.11.033


Jacob Jensen, Dyment Jerome, Yatheesh V. (2014). Revisiting the structure, age, and evolution of the Wharton Basin to better understand subduction under Indonesia. Journal Of Geophysical Research-solid Earth, 119(1), 169-190. https://doi.org/10.1002/2013JB010285


Maurin Thomas, Rangin Claude (2009). Impact of the 90 degrees E ridge at the Indo-Burmese subduction zone imaged from deep seismic reflection data. Marine Geology, 266(1-4), 143-155. https://doi.org/10.1016/j.margeo.2009.07.015


Maurin Thomas, Rangin Claude (2009). Structure and kinematics of the Indo-Burmese Wedge: Recent and fast growth of the outer wedge. Tectonics, 28(2/TC2010), 1-21. Publisher's official version : https://doi.org/10.1029/2008TC002276 , Open Access version : https://archimer.ifremer.fr/doc/00297/40802/


Cattin R., Chamot-Rooke N., Pubellier M., Rabaute A., Delescluse M., Vigny C., Fleitout L., Dubernet P. (2009). Stress change and effective friction coefficient along the Sumatra-Andaman-Sagaing fault system after the 26 December 2004 (M-w=9.2) and the 28 March 2005 (M-w=8.7) earthquakes. Geochemistry Geophysics Geosystems, 10(3), Q03011 - 1-21. Publisher's official version : https://doi.org/10.1029/2008GC002167 , Open Access version : https://archimer.ifremer.fr/doc/00297/40803/


Delescluse M., Montesi L. G. J., Chamotrooke Nicolas (2008). Fault reactivation and selective abandonment in the oceanic lithosphere. Geophysical Research Letters, 35(L16312), 1-5. Publisher's official version : https://doi.org/10.1029/2008GL035066 , Open Access version : https://archimer.ifremer.fr/doc/00237/34804/


Nielsen C, Chamot-Rooke N, Rangin C (2004). From partial to full strain partitioning along the Indo-Burmese hyper-oblique subduction. Marine Geology, 209(1-4), 303-327. https://doi.org/10.1016/j.margeo.2004.05.001