Deep-Water Sedimentary Characteristics and Response in the Reed Area of the Southern South China Sea
Zheng Hong-Bo; Pin, Yan; Wang, Yan-Lin; Xing, Yu-Qing
刊名MARINE GEORESOURCES & GEOTECHNOLOGY
2016
卷号34期号:2页码:162-168
关键词bottom current deep-water channel gravity flow reed area sediment waves
通讯作者Zheng, HB (reprint author), 164 West Xingang Rd, Guangzhou 510301, Guangdong, Peoples R China.
中文摘要Many researchers have focused on the characteristics of tectonic evolution in the Reed area of the southern South China Sea, but there has been little research focusing on deep-water sedimentary characteristics. Seismic data acquired in the Reed area have been processed and analyzed; representative deep-water sedimentary patterns, such as sediment waves, deep-water channels, slumping, and sliding mass, can be clearly distinguished from these seismic profiles. Combining this data with the geological setting and seafloor topography of the research area, it can be concluded that deep-water channels, slumping, and sliding depositions which have developed on the continental slope of the northeast Reed basin were formed by gravity flow, and the sediment waves which occur in the west and northwest Reed basin have been generated by deep-water bottom current.
学科主题Engineering; Oceanography; Mining & Mineral Processing
内容类型期刊论文
源URL[http://ir.scsio.ac.cn/handle/344004/15593]  
专题南海海洋研究所_中科院边缘海地质重点实验室
推荐引用方式
GB/T 7714
Zheng Hong-Bo,Pin, Yan,Wang, Yan-Lin,et al. Deep-Water Sedimentary Characteristics and Response in the Reed Area of the Southern South China Sea[J]. MARINE GEORESOURCES & GEOTECHNOLOGY,2016,34(2):162-168.
APA Zheng Hong-Bo,Pin, Yan,Wang, Yan-Lin,&Xing, Yu-Qing.(2016).Deep-Water Sedimentary Characteristics and Response in the Reed Area of the Southern South China Sea.MARINE GEORESOURCES & GEOTECHNOLOGY,34(2),162-168.
MLA Zheng Hong-Bo,et al."Deep-Water Sedimentary Characteristics and Response in the Reed Area of the Southern South China Sea".MARINE GEORESOURCES & GEOTECHNOLOGY 34.2(2016):162-168.
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