Submarine slide evidence for late Miocene strike-slip reversal of the Red River Fault
Wang DaWei1; Wu ShiGuo1; Li ChunFeng2; Yao GenShun3
2016-11-01
发表期刊SCIENCE CHINA-EARTH SCIENCES
卷号59期号:11页码:2231-2239
摘要During the late Miocene (similar to 5.5 Ma), a large-scale submarine slide with an area of approximately 18000 km(2) and a maximum thickness of 930 m formed in the deep-water region of the Qiongdongnan Basin. The large-scale submarine slide has obvious features in seismic profile, with normal faults in the proximal region, escarpments at the lateral boundary, and a pronounced shear surface at the base. The internal seismic reflections are chaotic and enclosed by parallel and sub-parallel seismic events. The main direction of sediment transport was from south to north and the main sediment source was the southern region of the Qiongdongnan Basin, which is located in the east of the Indo-China Peninsula and the north of the Guangle uplift. In this region, late Miocene strike-slip reversal of the Red River Fault, uplift and increased erosion of the Indo-China Peninsula, and an abrupt rise in the rate of deposition in the western part of the South China Sea provided the basic conditions and triggering mechanism for the large-scale submarine slide. The discovery of the large-scale submarine slide provides sedimentological evidence for the tectonic event of late Miocene strike-slip reversal of the Red River Fault. It can also be inferred that the greatest tectonic activity during the process of the Red River Fault reversal occurred at similar to 5.5 Ma from the age of top surface of the submarine slide.
文章类型Article
关键词Red River Fault Qiongdongnan Basin Deep-water Submarine Slide Seismic Reflection Character
WOS标题词Science & Technology ; Physical Sciences
DOI10.1007/s11430-015-5534-9
收录类别SCI
语种英语
关键词[WOS]SOUTH CHINA SEA ; QIONGDONGNAN BASIN ; TECTONIC SUBSIDENCE ; YINGGEHAI BASIN ; EVOLUTION
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000387396800013
引用统计
被引频次:3[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.idsse.ac.cn/handle/183446/1660
专题深海科学研究部_深海地球物理与资源研究室
作者单位1.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China
2.Zhejiang Univ, Ocean Coll, Zhoushan 310013, Peoples R China
3.PetroChina Hangzhou Inst Geol, Hangzhou 310023, Zhejiang, Peoples R China
第一作者单位中国科学院深海科学与工程研究所
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Wang DaWei,Wu ShiGuo,Li ChunFeng,et al. Submarine slide evidence for late Miocene strike-slip reversal of the Red River Fault[J]. SCIENCE CHINA-EARTH SCIENCES,2016,59(11):2231-2239.
APA Wang DaWei,Wu ShiGuo,Li ChunFeng,&Yao GenShun.(2016).Submarine slide evidence for late Miocene strike-slip reversal of the Red River Fault.SCIENCE CHINA-EARTH SCIENCES,59(11),2231-2239.
MLA Wang DaWei,et al."Submarine slide evidence for late Miocene strike-slip reversal of the Red River Fault".SCIENCE CHINA-EARTH SCIENCES 59.11(2016):2231-2239.
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