Margin deltas in the northern part of the Red River basin
Margin deltas are the last ones that were formed in a shelf break zone, when a sea level has slowdown during last time of a forced regression and the beginning of the success transgression. The margin deltas are abruptly thickened in the zone of shelf break, became thinner landward and basinward. Be...
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VNU
2014
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oai:112.137.131.14:11126-45662017-08-11T04:55:04Z Margin deltas in the northern part of the Red River basin Doan, Dinh Lam Nguyen, Trong Tin Nguyen, Thi Hong Margin delta Delta front deposit Red River basin Margin deltas are the last ones that were formed in a shelf break zone, when a sea level has slowdown during last time of a forced regression and the beginning of the success transgression. The margin deltas are abruptly thickened in the zone of shelf break, became thinner landward and basinward. Because they were formed inthe shelf edge, they have a relatively high sand/clay ratio, prone to turbidite. In the northern part of the Red River basin, during the Miocene the margin deltas had developed eastward from the plot 103, i.e. from theborehole 103-TH-1X, 103-TG-1X and 103-HOL seaward. An existence of the margin deltas in this region confirms a presence of the basin floor fans in the central part of basin - very important objects for oil-gas prospecting. 2014-03-18T06:14:06Z 2015-08-14T08:55:18Z 2014-03-18T06:14:06Z 2015-08-14T08:55:18Z 2008 Article p. 16-25 http://repository.vnu.edu.vn/handle/11126/4566 en application/pdf VNU |
| institution |
Đại học Quốc Gia Hà Nội |
| collection |
DSpace |
| language |
English |
| topic |
Margin delta Delta front deposit Red River basin |
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Margin delta Delta front deposit Red River basin Doan, Dinh Lam Nguyen, Trong Tin Nguyen, Thi Hong Margin deltas in the northern part of the Red River basin |
| description |
Margin deltas are the last ones that were formed in a shelf break zone, when a sea level has slowdown during last time of a forced regression and the beginning of the success transgression. The margin deltas are abruptly thickened in the zone of shelf break, became thinner landward and basinward. Because they were formed inthe shelf edge, they have a relatively high
sand/clay ratio, prone to turbidite.
In the northern part of the Red River basin, during the Miocene the margin deltas had
developed eastward from the plot 103, i.e. from theborehole 103-TH-1X, 103-TG-1X and 103-HOL seaward.
An existence of the margin deltas in this region confirms a presence of the basin floor fans in the central part of basin - very important objects for oil-gas prospecting. |
| format |
Article |
| author |
Doan, Dinh Lam Nguyen, Trong Tin Nguyen, Thi Hong |
| author_facet |
Doan, Dinh Lam Nguyen, Trong Tin Nguyen, Thi Hong |
| author_sort |
Doan, Dinh Lam |
| title |
Margin deltas in the northern part of the Red River basin |
| title_short |
Margin deltas in the northern part of the Red River basin |
| title_full |
Margin deltas in the northern part of the Red River basin |
| title_fullStr |
Margin deltas in the northern part of the Red River basin |
| title_full_unstemmed |
Margin deltas in the northern part of the Red River basin |
| title_sort |
margin deltas in the northern part of the red river basin |
| publisher |
VNU |
| publishDate |
2014 |
| url |
http://repository.vnu.edu.vn/handle/11126/4566 |
| work_keys_str_mv |
AT doandinhlam margindeltasinthenorthernpartoftheredriverbasin AT nguyentrongtin margindeltasinthenorthernpartoftheredriverbasin AT nguyenthihong margindeltasinthenorthernpartoftheredriverbasin |
| _version_ |
1787734778577944576 |