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Fluvial system development and subsequent marine transgression in Yellow River (Huanghe) delta and its adjacent sea regions during last glacial maximum to early Holocene

文献类型：期刊论文

作者Zhou, Liangyong1,2; Liu, Jian1,2; Saito, Yoshiki3; Liu, J. Paul4; Li, Guangxue5; Liu, Qingsong6; Gao, Maosheng1,2; Qiu, Jiandong1,2
刊名CONTINENTAL SHELF RESEARCH
出版日期2014-11-01
卷号90页码:117-132
关键词Holocene transgression Paleotopography Fluvial sediment Bohai Sea North Yellow Sea Yellow River delta
ISSN号0278-4343
DOI10.1016/j.csr.2014.06.012
文献子类Article
英文摘要Paleotopography of the Yellow River (Huanghe) delta area and the western Bohai Sea during the last glacial maximum (LGM) is important to understand fluvial activities of the Yellow River linked with the LGM climate. By integrating data sets of both onshore and offshore borehole cores and offshore high-resolution seismic profiles, we reconstructed the paleotopography of this area from the LGM to the early Holocene. The fluvial sediment fades of the LGM identified in these cores was characterized by poorly sorted medium- to coarse-grained sands, which shows chaotic patterns in seismic profiles. REE characteristics and clay mineral components of the fluvial sediments suggest that they were derived mostly from the paleo-Yellow River. The basal and top bounding surfaces of the fluvial sediments slope very gently toward the northeast, similar to the present morphology of the North China Plain formed by the Yellow River. No incised valley morphology is detected in the basal topography, because of the long distance from the study area to the paleoshoreline during the LGM, and also because of the very gentle gradient of the paleo-Yellow River from the northern part of North China Plain to the continental shelf area, with concave-upward morphology. Aggradational stacking of the fluvial sediments over the entire North China Plain and in the study area indicates that the Yellow River flowed in these areas during the LGM to the early Holocene. The Holocene marine and coastal sediments onlap onto the underlying fluvial sediments. These basal marine or brackish sediments are diachronous from offshore areas of the Bohai Sea to the Yellow River delta area, with older sediments in the east and younger sediments in the west, which clearly reflects the early Holocene marine transgression from the North Yellow Sea to the Bohai Sea. (C) 2014 Elsevier Ltd. All rights reserved.
WOS关键词BOHAI SEA ; SUBAQUEOUS DELTA ; SOUTHEAST-ASIA ; CHINA ; SEDIMENTATION ; EVOLUTION ; SHELF ; BAY
WOS研究方向Oceanography
语种英语
WOS记录号WOS:000347606000013
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China(41330964 ; National Natural Science Foundation of China(41330964 ; China Geological Survey(1212011120172 ; China Geological Survey(1212011120172 ; National Basic Research Program of China(2005CB422304) ; National Basic Research Program of China(2005CB422304) ; Marine Safeguard Project(GZH201200503) ; Marine Safeguard Project(GZH201200503) ; '100 Talent Program' of the Chinese Academy of Sciences ; '100 Talent Program' of the Chinese Academy of Sciences ; 41240022) ; 41240022) ; 1212010611402) ; 1212010611402) ; National Natural Science Foundation of China(41330964 ; National Natural Science Foundation of China(41330964 ; China Geological Survey(1212011120172 ; China Geological Survey(1212011120172 ; National Basic Research Program of China(2005CB422304) ; National Basic Research Program of China(2005CB422304) ; Marine Safeguard Project(GZH201200503) ; Marine Safeguard Project(GZH201200503) ; '100 Talent Program' of the Chinese Academy of Sciences ; '100 Talent Program' of the Chinese Academy of Sciences ; 41240022) ; 41240022) ; 1212010611402) ; 1212010611402) ; National Natural Science Foundation of China(41330964 ; National Natural Science Foundation of China(41330964 ; China Geological Survey(1212011120172 ; China Geological Survey(1212011120172 ; National Basic Research Program of China(2005CB422304) ; National Basic Research Program of China(2005CB422304) ; Marine Safeguard Project(GZH201200503) ; Marine Safeguard Project(GZH201200503) ; '100 Talent Program' of the Chinese Academy of Sciences ; '100 Talent Program' of the Chinese Academy of Sciences ; 41240022) ; 41240022) ; 1212010611402) ; 1212010611402) ; National Natural Science Foundation of China(41330964 ; National Natural Science Foundation of China(41330964 ; China Geological Survey(1212011120172 ; China Geological Survey(1212011120172 ; National Basic Research Program of China(2005CB422304) ; National Basic Research Program of China(2005CB422304) ; Marine Safeguard Project(GZH201200503) ; Marine Safeguard Project(GZH201200503) ; '100 Talent Program' of the Chinese Academy of Sciences ; '100 Talent Program' of the Chinese Academy of Sciences ; 41240022) ; 41240022) ; 1212010611402) ; 1212010611402)
源URL[http://ir.iggcas.ac.cn/handle/132A11/85628]  
专题中国科学院地质与地球物理研究所
通讯作者Zhou, Liangyong
作者单位1.Minist Land & Resources, Key Lab Marine Hydrocarbon Resources & Environm G, Qingdao 266071, Peoples R China
2.Qingdao Inst Marine Geol, Qingdao 266071, Peoples R China
3.Geol Survey Japan, AIST, Tsukuba, Ibaraki 3058567, Japan
4.N Carolina State Univ, Dept Marine Earth & Atmospher Sci, Raleigh, NC 27605 USA
5.Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, Paleomagnetism & Geochronol Lab SKL LE, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Zhou, Liangyong,Liu, Jian,Saito, Yoshiki,et al. Fluvial system development and subsequent marine transgression in Yellow River (Huanghe) delta and its adjacent sea regions during last glacial maximum to early Holocene[J]. CONTINENTAL SHELF RESEARCH,2014,90:117-132.
APA Zhou, Liangyong.,Liu, Jian.,Saito, Yoshiki.,Liu, J. Paul.,Li, Guangxue.,...&Qiu, Jiandong.(2014).Fluvial system development and subsequent marine transgression in Yellow River (Huanghe) delta and its adjacent sea regions during last glacial maximum to early Holocene.CONTINENTAL SHELF RESEARCH,90,117-132.
MLA Zhou, Liangyong,et al."Fluvial system development and subsequent marine transgression in Yellow River (Huanghe) delta and its adjacent sea regions during last glacial maximum to early Holocene".CONTINENTAL SHELF RESEARCH 90(2014):117-132.

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来源：地质与地球物理研究所

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