tailieunhanh - Reconstruction of the holocene paleo geography of the the Mekong river Delta, Vietnam

The paleo-geographical reconstructions are obtained from the interpolated MRD sea-level curve, depositional facies and Pleistocene surface topography of the former and new cores in the MRD and surrouding shallow offshore. The paleo-geography of the MRD is distinguished by four stages corresponding to sea-levels of -32m/10 ka, -4m/, + and +1m/ ka. |