Rifting process and formation mechanisms of syn-rift stage prolongation in the deepwater basin, northern South China Sea View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2008-12

AUTHORS

DongDong Dong, ShiGuo Wu, GongCheng Zhang, ShengQiang Yuan

ABSTRACT

Based on the latest seismic and geological data, tectonic subsidence of three seismic lines in the deepwater area of Pearl River Mouth Basin (PRMB), the northern South China Sea (SCS), is calculated. The result shows that the rifting process of study area is different from the typical passive continental margin basin. Although the seafloor spreading of SCS initiated at 32 Ma, the tectonic subsidence rate does not decrease but increases instead, and then decreases at about 23 Ma, which indicates that the rifting continued after the onset of seafloor spreading until about 23 Ma. The formation thickness exhibits the same phenomenon, that is the syn-rift stage prolonged and the post-rift thermal subsidence delayed. The formation mechanisms are supposed to be three: (1) the lithospheric rigidity of the northern SCS is weak and its ductility is relatively strong, which delayed the strain relaxation resulting from the seafloor spreading; (2) the differential layered independent extension of the lithosphere may be one reason for the delay of post-rift stage; and (3) the southward transition of SCS spreading ridge during 24 to 21 Ma and the corresponding acceleration of seafloor spreading rate then triggered the initiation of large-scale thermal subsidence in the study area at about 23 Ma. More... »

PAGES

3715-3725

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s11434-008-0326-1

DOI

http://dx.doi.org/10.1007/s11434-008-0326-1

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1049472732


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136 https://www.grid.ac/institutes/grid.497420.c schema:alternateName China University of Petroleum
137 schema:name China University of Petroleum, 266555, Qingdao, China
138 Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, 266071, Qingdao, China
139 rdf:type schema:Organization
 




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