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Abstract
The TV1 boring site is a typical section at coastal part of the Mekong River Delta (MRD) and has 20.8m in thickness of the Holocene deltaic sediments. Holocene marine transgressive deposit is not found here. Holocene deltaic sediments unconformably covered late Pleistocene sediments and characterized by 20,8 m in thickness of the coarsening-upward succession including pro-delta, delta front, sub- to intertidal flat and beach ridge sediments. This typical section has been dated since 3 ky. BP. It is a typical tide- and wave- dominated delta succession of the MRD.
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Article Details
Issue: Vol 8 No 8 (2005)
Page No.: 56-62
Published: Aug 31, 2005
Section: Article
DOI: https://doi.org/10.32508/stdj.v8i8.3057
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Copyright: The Authors. This is an open access article distributed under the terms of the Creative Commons Attribution License CC-BY 4.0., which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
How to Cite
Van Lap, N., & Kim Oanh, T. (2005). HOLOCENE SEDIMENTARY FACIES CHANGE IN TV1 CORE MEKONG RIVER DELTA. Science and Technology Development Journal, 8(8), 56-62. https://doi.org/https://doi.org/10.32508/stdj.v8i8.3057
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