Now showing items 1-4 of 4
Neogene syn-tectonic sedimentation in the eastern margin of Arakan-Bengal basins, and its implications on for the Indian-Asian collision in western Myanmar
(Gondwana Research, 2014)
The Arakan Basin is one of the major sedimentary basins formed in the frontal part of the Himalayan orogenic belt since the Late Cenozoic. Defining one of the four major sedimentary basins of Myanmar, it is geomorphologically ...
1320525 Neogene Sedimentary Fringe, West of Indo-Burma Ranges in Western Myanmar: Some Evidences for Late Cenozoic Synorogenic Sedimentation in Himalayan-Bengal System
The Arakan Basin is one of the representative clastic basins formed in the frontal part of the Himalayan orogenic belt since the Late Cenozoic. Defining one of the four major sedimentary basins of Myanmar, it is ...
Embankment failures related with bedrock slides in the Shimanto Belt, south Kyushu, Japan
(Journal of the Japan Landslide Society, 2003)
Marine transgression and regression in Miocene sequences of northern Pegu (Bago) Yoma, Central Myanmar
(Journal of Asian Earth Sciences, 1999)
Neogene strata of the northern part of the Pegu (Bago) Yoma Range, Cent ral Myanmar , con ta in a series of shallow marine clastic sediments with stratigraphic ages ranging from the Earl y to Late Miocene. The studied ...