干旱区生态环境知识资源中心(Arid): Alternating of aggradation and progradation dominated clinothems and its implications for sediment delivery to deep lake: The Eocene Dongying Depression, Bohai Bay Basin, east China

Arid

DOI	10.1016/j.marpetgeo.2019.104197
	Alternating of aggradation and progradation dominated clinothems and its implications for sediment delivery to deep lake: The Eocene Dongying Depression, Bohai Bay Basin, east China
	Liu, Jianping; Xian, Benzhong; Ji, Youliang; Gong, Chenglin; Wang, Junhui; Wang, Zhen; Chen, Peng; Song, Delin; Wei, Wenzong; Zhang, Ximeng; Dou, Luxing
通讯作者	Xian, BZ
来源期刊	MARINE AND PETROLEUM GEOLOGY
ISSN	0264-8172
EISSN	1873-4073
出版年	2020
卷号	114
英文摘要	Sediment routing in deep-water settings can be significantly different in lacustrine basins from their well-studied marine counterparts, which has been largely overlooked during the past decades. The seismically well-imaged lacustrine clinothems in the Eocene Dongying Depression provide a good opportunity to bridge the deep-water sediment partitioning with clinothem architecture and shelf-edge trajectories, which have been studied through the integration of 3D seismic data and well-logging data. In the study area, the Eocene delta-complexes are architecturally manifested as alternating aggradation dominated (AC) and progradation dominated clinothems (PC). The Eocene Dongying clinothem architecture has been documented in terms of shelf-edge trajectory angle (theta(sht)), edge-to-toe distance (ETT), aggradation height (Ah), progradation distance (Pd) and maximum foreset angle (gamma(mfa)). Aggradation dominated clinothems are characterized by ascending shelf-edge trajectories with thick and widespread sand-prone bottomsets, suggesting higher efficiency of sediment delivery into the outlying lake floor. Progradation dominated clinothems, in contrast, are characterized by flat to slightly descending trajectories and generally by a lack of bottomsets. Alternations of rising and flat to slightly descending trajectories accompanied with different clinothem types probably indicate frequent relative lake level changes (on time-scales of 100s of kyr). Further analysis of seismic images and extensive well-logs suggest the distal aggradational bottomsets are generally consist of sub-lacustrine channel-lobe systems, whereas sediment slide, slump blocks occur in slope to slope toe areas of progradation dominated clinothems, which indicate varied processes of deep-water sediment transport associated with different clinothem types and shelf-edge trajectories. Lake-level, sediment supply, water salinity and density change induced by humid-arid climate cycle are suggested to be main factors controlling clinothems stacking pattern and sediment dispersal into deep-lacustrine. Humid climate are considered to be related with strongly aggradational clinothems, during which sediment can be directly transported to the distant bottomset areas due to increased sediment concentration and energy in river discharge. Whereas during dry periods, progradation dominated clinothems start to build under stillstand or falling lake level conditions, sediment generally accumulates at river mouth and collapses due to sediment overload or fault activity. Therefore, a relationship between deep-lacustrine depositional process and climatic signature was established which may provide new thoughts in both the study of deep-water sequences and deep water exploration in lacustrine basins.
英文关键词	Lacustrine clinothem Lake level Climate change Deep-water sand Bohai Bay Basin
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000514747800006
WOS关键词	SEQUENCE STRATIGRAPHIC MODEL ; SHELF-MARGIN CLINOFORMS ; SEISMIC GEOMORPHOLOGY ; TRAJECTORY ANALYSIS ; DEPOSITIONAL MODEL ; TURBIDITY CURRENTS ; SHAHEJIE FORMATION ; CLIMATIC CONTROL ; SUBMARINE FANS ; LEVEL CHANGE
WOS类目	Geosciences, Multidisciplinary
WOS研究方向	Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/324306
作者单位	[Liu, Jianping; Xian, Benzhong; Ji, Youliang; Gong, Chenglin; Wang, Junhui; Chen, Peng; Song, Delin; Wei, Wenzong; Zhang, Ximeng; Dou, Luxing] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China; [Liu, Jianping; Xian, Benzhong; Ji, Youliang; Gong, Chenglin; Wang, Junhui] China Univ Petr, Coll Geosci, Beijing 102249, Peoples R China; [Wang, Zhen] China Univ Geosci Beijing, Sch Energy Resources, Beijing 100083, Peoples R China
推荐引用方式 GB/T 7714	Liu, Jianping,Xian, Benzhong,Ji, Youliang,et al. Alternating of aggradation and progradation dominated clinothems and its implications for sediment delivery to deep lake: The Eocene Dongying Depression, Bohai Bay Basin, east China[J],2020,114.
APA	Liu, Jianping.,Xian, Benzhong.,Ji, Youliang.,Gong, Chenglin.,Wang, Junhui.,...&Dou, Luxing.(2020).Alternating of aggradation and progradation dominated clinothems and its implications for sediment delivery to deep lake: The Eocene Dongying Depression, Bohai Bay Basin, east China.MARINE AND PETROLEUM GEOLOGY,114.
MLA	Liu, Jianping,et al."Alternating of aggradation and progradation dominated clinothems and its implications for sediment delivery to deep lake: The Eocene Dongying Depression, Bohai Bay Basin, east China".MARINE AND PETROLEUM GEOLOGY 114(2020).