Sedimentary evolution of the Holocene subaqueous clinoform off the southern Shandong Peninsula in the Western South Yellow Sea

2014 ◽  
Vol 13 (5) ◽  
pp. 747-760 ◽  
Author(s):  
Jiandong Qiu ◽  
Jian Liu ◽  
Yoshiki Saito ◽  
Zigeng Yang ◽  
Baojing Yue ◽  
...  
Keyword(s):  
Yellow Sea ◽  
South Yellow Sea ◽  
Shandong Peninsula ◽  
The Holocene ◽  
Sedimentary Evolution

Sedimentary evolution of the Holocene subaqueous clinoform off the Shandong Peninsula in the Yellow Sea

2007 ◽  
Vol 236 (3-4) ◽  
pp. 165-187 ◽  
Author(s):  
Jian Liu ◽  
Yoshiki Saito ◽  
Hong Wang ◽  
Zigeng Yang ◽  
Rei Nakashima
Keyword(s):  
Yellow Sea ◽  
The Yellow Sea ◽  
Shandong Peninsula ◽  
The Holocene ◽  
Sedimentary Evolution

11000-Year Record of Trace Metals in Sediments off the Southern Shandong Peninsula in the South Yellow Sea

2020 ◽  
Vol 19 (6) ◽  
pp. 1307-1314
Author(s):  
Jiandong Qiu ◽  
Jinqing Liu ◽  
Meina Li ◽  
Ke Cao ◽  
Shuang Wang ◽  
...  
Keyword(s):  
Trace Metals ◽  
Yellow Sea ◽  
South Yellow Sea ◽  
The South ◽  
Shandong Peninsula ◽  
The South Yellow Sea

Textures, provenances and structures of sediment in the inner shelf south of Shandong Peninsula, western South Yellow Sea

2018 ◽  
Vol 212 ◽  
pp. 153-163 ◽  
Author(s):  
Gang Hu ◽  
Kehui Xu ◽  
Peter D. Clift ◽  
Yong Zhang ◽  
Yuting Li ◽  
...  
Keyword(s):  
Yellow Sea ◽  
South Yellow Sea ◽  
Inner Shelf ◽  
Shandong Peninsula

scholarly journals Geochemistry and Holocene Sedimentary Environment Evolution of Subaqueous Clinoform off Shandong Peninsula (Yellow Sea)

Minerals ◽  
2021 ◽  
Vol 11 (11) ◽  
pp. 1209
Author(s):  
Yingtao Zhu ◽  
Yongchen Xu ◽  
Mingyang Liu ◽  
Zhaobin Lin ◽  
Longhai Zhu
Keyword(s):  
Deposition Rate ◽  
Yellow Sea ◽  
Sedimentary Environment ◽  
River Sediments ◽  
Source Area ◽  
Sediment Provenance ◽  
14C Dating ◽  
Sediment Grain Size ◽  
Shandong Peninsula ◽  
The Holocene

As a key sedimentary body connecting the north and South Yellow Sea, the subaqueous clinoform off Shandong Peninsula plays an important role in the sedimentary system of China seas, and it is also a studied example in the study among the major “source to sink” systems. Based on AMS 14C dating, sediment grain size, major and trace element contents from core WH-05 located at the edge of the clinoform, we discuss changes in the deposition rate, analyze sediment provenance and controlling factors, and reveal the environmental evolution of the source area since the Holocene. Results from core WH-05 show that marine sedimentation began at about 8.5 ka B.P. The deposition rate decreased from the initial 28.37 m/ka to 0.52 m/ka. Sediment provenance suggests that the Huanghe river sediments have been the main source for the study area since the Holocene. The As/Al, V/Sc indicators show that the environmental oxidation environment was gradually weakened and then increased slightly starting from 7.0 ka B.P. The change in redox is consistent with the change in sea level, the deposition rate, and depositional depth.

A DISCUSSION ON MARINE MESOZOIC-PALAEOZOIC RESERVOIRS IN SOUTH YELLOW SEA

2011 ◽  
Vol 31 (5) ◽  
pp. 101-108 ◽  
Author(s):  
Jie LIANG ◽  
Yinguo ZHANG ◽  
Gang DONG ◽  
Binhui XIONG
Keyword(s):  
Yellow Sea ◽  
South Yellow Sea
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