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The evolution of the slope breaks in Qiongdongnan Basin and their controlling factors
Liu, Jianbao; Sun, Zhen; Wang, Zhenfeng; Sun, Zhipeng; Wang, Zhangwen; Zhao, Zhongxian; Liu, Siqing; liujianbao342@126.com; zhensun@scsio.ac.cn
2015
Source PublicationMARINE GEOPHYSICAL RESEARCH
Volume36Issue:2-3Pages:211-226
Subtype0025-3235
AbstractQiongdongnan Basin (QB) experienced three main tectonic stages in the Cenozoic: rifting, thermal subsidence, and accelerated subsidence. Corresponding to these stages, the slope breaks also underwent three different evolutionary stages, which differed in space and time between the east and west of QB. Structural slope breaks developed during the rifting stage in the Paleocene. Transitional sedimentary strata without obvious slope break developed in the neritic environment during the thermal subsidence stage in the Neocene. Sedimentary slope breaks and gentle slope zone without slope break developed during the accelerated subsidence stage. The sedimentary slope breaks could be further classified into progradational and aggradational types, the starting points of which varied in space and time. Spatially, the progradational sequences in the Ledong and Lingshui sags started at the north of today's deep central basin, distant from the basin edge. In the Songnan and Baodao sags, the aggradational sequences were close to the sag edge and essentially controlled by the underlying major boundary faults. Temporally, sedimentary slope breaks developed early in the east and late in the west and were initially partitioned and eventually unified. Fault activity controlled the types and ending time of structural slope breaks during the rifting stage, while tectonic subsidence controlled the time and places of progradational slope breaks during the accelerated subsidence stage. Sediment supply controlled the superposition patterns of the sedimentary sequences of the sedimentary slope breaks. It is suggested that the evolutionary history of the slope breaks has been primarily affected by the southward transition of the South China Sea ocean ridge, the westward collision of the Philippine Sea Plate, and the dextral strike-slipping of the Red River Fault.
Department[Liu, Jianbao] Henan Inst Engn, Sch Resource & Environm, Zhengzhou 451191, Peoples R China; [Liu, Jianbao; Sun, Zhen; Wang, Zhenfeng; Zhao, Zhongxian; Liu, Siqing] Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China; [Wang, Zhenfeng; Sun, Zhipeng] China Natl Offshore Oil Corp, Western Branch, Zhanjiang 524000, Guangdong, Peoples R China ; LTO
KeywordSlope Breaks Qiongdongnan Basin Fault No. 2 Tectonic Subsidence
Subject AreaGeochemistry & Geophysics ; Oceanography
Indexed BySCI
Document Type期刊论文
Identifierhttp://ir.scsio.ac.cn/handle/344004/15042
Collection热带海洋环境国家重点实验室(LTO)
Corresponding Authorliujianbao342@126.com; zhensun@scsio.ac.cn
Recommended Citation
GB/T 7714
Liu, Jianbao,Sun, Zhen,Wang, Zhenfeng,et al. The evolution of the slope breaks in Qiongdongnan Basin and their controlling factors[J]. MARINE GEOPHYSICAL RESEARCH,2015,36(2-3):211-226.
APA Liu, Jianbao.,Sun, Zhen.,Wang, Zhenfeng.,Sun, Zhipeng.,Wang, Zhangwen.,...&zhensun@scsio.ac.cn.(2015).The evolution of the slope breaks in Qiongdongnan Basin and their controlling factors.MARINE GEOPHYSICAL RESEARCH,36(2-3),211-226.
MLA Liu, Jianbao,et al."The evolution of the slope breaks in Qiongdongnan Basin and their controlling factors".MARINE GEOPHYSICAL RESEARCH 36.2-3(2015):211-226.
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