Late Pleistocene-Holocene sequence stratigraphy of the subaqueous Red River delta and the adjacent shelf

Nguyen Trung Thanh, Paul Jing Liu, Mai Duc Dong, Dang Hoai Nhon, Do Huy Cuong, Bui Viet Dung, Phung Van Phach, Tran Duc Thanh, Duong Quoc Hung, Ngo Thanh Nga
Author affiliations


  • Nguyen Trung Thanh Institute of Marine Geology and Geophysics (VAST), Hanoi, Vietnam
  • Paul Jing Liu Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA
  • Mai Duc Dong Institute of Marine Geology and Geophysics (VAST), Hanoi, Vietnam
  • Dang Hoai Nhon Institute of Marine Environment and Resources (VAST), Haiphong, Vietnam
  • Do Huy Cuong Institute of Marine Geology and Geophysics (VAST), Hanoi, Vietnam
  • Bui Viet Dung Vietnam Petroleum Institute, 173-Trung Kinh, Hanoi, Vietnam
  • Phung Van Phach Institute of Marine Geology and Geophysics (VAST), Hanoi, Vietnam
  • Tran Duc Thanh Institute of Marine Environment and Resources (VAST), Hai Phong, Vietnam
  • Duong Quoc Hung Institute of Marine Geology and Geophysics (VAST), Hanoi, Vietnam
  • Ngo Thanh Nga Institute of Geography (VAST), Hanoi, Vietnam



Sequence stratigraphy, Systems tracts, Red River delta, Sedimentary evolution, Sedimentary facies


The model of Late Pleistocene-Holocene sequence stratigraphy of the subaqueous Red River delta and the adjacent shelf is proposed by interpretation of high-resolution seismic documents and comparison with previous research results on Holocene sedimentary evolution on the delta plain. Four units (U1, U2, U3, and U4) and four sequence stratigraphic surfaces (SB1, TS, TRS and MFS) were determined. The formation of these units and surfaces is related to the global sea-level change in Late Pleistocene-Holocene. SB1, defined as the sequence boundary, was generated by subaerial processes during the Late Pleistocene regression and could be remolded partially or significantly by transgressive ravinement processes subsequently. The basal unit U1 (fluvial formations) within incised valleys is arranged into the lowstand systems tract (LST) formed in the early slow sea-level rise ~19-14.5 cal.kyr BP, the U2 unit is arranged into the early transgressive systems tract (E-TST) deposited mainly within incised-valleys under the tide-influenced river to estuarine conditions in the rapid sea-level rise ~14.5-9 cal.kyr BP, the U3 unit is arranged into the late transgressive systems tract (L-TST) deposited widely on the continental shelf in the fully marine condition during the late sea-level rise ~9-7 cal.kyr BP, and the U4 unit represents for the highstand systems tract (HST) with clinoform structure surrounding the modern delta coast, extending to the water depth of 25-30 m, developed by sediments from the Red River system in ~3-0 cal.kyr BP.


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How to Cite

Thanh, N. T., Liu, P. J., Dong, M. D., Nhon, D. H., Cuong, D. H., Dung, B. V., Phach, P. V., Thanh, T. D., Hung, D. Q., & Nga, N. T. (2018). Late Pleistocene-Holocene sequence stratigraphy of the subaqueous Red River delta and the adjacent shelf. Vietnam Journal of Earth Sciences, 40(3), 271–287.




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