| Summary: | International audience Sedimentary basins in Myanmar have recorded key events of the India-Asia collision including associated geody-namic movements and paleoclimatic records. In particular, Paleogene deposits provide invaluable insight on theaccretion of the Burma terrane, its rotation associated with the alleged extrusion of Indochina and the formation ofthe Indo-Burman ranges. They also yield unique records of monsoonal intensity during the growth of the TibetanPlateau and a rich paleontological assemblage including some of the earliest primates. However, understanding thepotential relations between these recorded events is strongly hindered by insufficient age control on these deposits.As part of the Myanmar Geodynamic & Paleoclimate Initiative and the ERC “MAGIC” project, our initial focusis to date Paleogene deposits of Myanmar with better accuracy using magnetostratigraphy. We present prelimi-nary results from the Chindwin Basin where we sampled a 400-meter section of the top of the Yaw formationrecording a major sedimentological facies transition previously estimated roughly as Eocene to Oligocene in age.Detailed rock magnetic analyses enabled to identify and isolate primary Characteristic Remanent Magnetizationsof normal and reversed polarities carried by iron sulfides, iron carbonates and/or iron oxides. A correlation tothe Geomagnetic Polarity Time Scale can be proposed suggesting deposition between the base of chrons C16n2nand the base of C13r (36.3 and 34.8 Ma). This age suggests the facies transition may be more likely associatedwith regional tectonics such as the Indo-Burman uplift rather than sea-level drop linked to ice-sheet formation atthe Eocene-Oligocene Transition at 33.9 Ma. In addition, the mean observed paleomagnetic declination (13.3+/-3.7) is statistically indistinguishable from declinations expected by geodynamic models with limited vertical-axisrotations of the Burma terrane and therefore supports little to no rotational extrusion since 35 Ma
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