Acoustical facies analysis at the Ba Lat delta front (Red River Delta, North Vietnam)

Title:	Acoustical facies analysis at the Ba Lat delta front (Red River Delta, North Vietnam)
Authors:	G.D. van den Bergh Tj.C.E. van Weering J.F. Boels D.M. Duc M.T. Nhuan
Keywords:	holocene acoustic facies recent sedimentation bottom sampling Red River Delta Vietnam
Issue Date:	2007
Publisher:	PERGAMON-ELSEVIER SCIENCE LTD, THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
Citation:	ISIKNOWLEDGE
Abstract:	A shallow penetrating, high-resolution acoustic study was performed in the Ba Lat delta, the major distributary of the Red River System in Northern Vietnam. An acoustic facies map was constructed and the various facies types were validated through analysis of bottom sediments, by a study of gravity cores collected at 22 stations. Analysis of the acoustic profiles and gravity cores revealed the presence of an asymmetrical, S to SW prograding prodelta lobe, in accordance with the prevailing longshore currents to the S. The southern part of this prodelta is detached from the protruding Ba Lat delta front. The prodelta is dominated by muddy sediments with minor thin (< 5 cm) sandy and silty layers. The coarser-grained layers decrease in abundance away from the Ba Lat river mouth. Offshore, the modern delta deposits are characterized by an off-lapping contact over a semi-prolonged bottom reflector lacking any sub-bottom reflectors. This semi-prolonged bottom reflector is correlated with sandy deposits of presumably Early Holocene age. Bottom and coastal erosion is restricted to two areas N and SW of the Ba Lat. Erosion in the North is inferred to be due to reduced sediment supply as a result of shifting in 1971 of the main outlet to its present, more southern location. The erosional area along the Hai Hau coast SW of the Ba Lat also has experienced a reduction in sediment supply in the course of the 20th century, when the local Song Vop distributary channel became less active and was completely dammed in the 1970s. Most sediment supplied by the Ba Lat at present bypasses the Hai Hau erosional coastal zone, as the active part of the Ba Lat prodelta is detached from the coast SW of the Ba Lat. An active, NNE-SSW trending fault system with surface expression is located along the offshore edge of the prodelta, and is linked to deeper fault structures in this active neotectonic region. Subsurface reflectors are folded in the vicinity of the fault. (c) 2006 Elsevier Ltd. All rights reserved.
Description:	JOURNAL OF ASIAN EARTH SCIENCES Volume: 29 Issue: 4 Pages: 532-544 Published: FEB 15 2007 ; TNS07648
URI:	http://www.sciencedirect.com/science/article/pii/S1367912006000782 http://repository.vnu.edu.vn/handle/VNU_123/31863
ISSN:	1367-9120
Appears in Collections:	Bài báo của ĐHQGHN trong Web of Science