Spatial distribution of hydrocarbon reservoirs in the West Korea Bay Basin in the northern part of the Yellow Sea, estimated by 3-D gravity forward modelling

2016 ◽  
Vol 208 (1) ◽  
pp. 75-85 ◽  
Author(s):  
Sungchan Choi ◽  
In-Chang Ryu ◽  
H.-J. Götze ◽  
Y. Chae
Keyword(s):  
Spatial Distribution ◽  
Yellow Sea ◽  
Hydrocarbon Reservoirs ◽  
The Yellow Sea ◽  
Forward Modelling ◽  
The West ◽  
Gravity Forward Modelling

scholarly journals Datasets on the spatial distribution of mercury and its controlling factors in the Yellow Sea

Data in Brief ◽  
2021 ◽  
Vol 35 ◽  
pp. 106792
Author(s):  
Do Hyun Jeong ◽  
Wooyoung Jeong ◽  
Saehun Baeg ◽  
Jihun Kim
Keyword(s):  
Spatial Distribution ◽  
Yellow Sea ◽  
Controlling Factors ◽  
The Yellow Sea

Tempo-spatial distribution and species diversity of green algae micro-propagules in the Yellow Sea during the large-scale green tide development

Harmful Algae ◽  
2014 ◽  
Vol 39 ◽  
pp. 40-47 ◽  
Author(s):  
Yan Li ◽  
Wei Song ◽  
Jie Xiao ◽  
Zongling Wang ◽  
Mingzhu Fu ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
Species Diversity ◽  
Green Algae ◽  
Yellow Sea ◽  
Large Scale ◽  
The Yellow Sea ◽  
Green Tide

scholarly journals Modeling the Oceanographic Impacts on the Spatial Distribution of Common Cephalopods During Autumn in the Yellow Sea

2020 ◽  
Vol 7 ◽  
Author(s):  
Yue Jin ◽  
Xianshi Jin ◽  
Harry Gorfine ◽  
Qiang Wu ◽  
Xiujuan Shan
Keyword(s):  
Spatial Distribution ◽  
Yellow Sea ◽  
The Yellow Sea

The Neolithic Age in Northern China

Antiquity ◽  
1933 ◽  
Vol 7 (28) ◽  
pp. 389-404 ◽  
Author(s):  
Carl Whiting Bishop
Keyword(s):  
Eastern Europe ◽  
Yellow Sea ◽  
Northern China ◽  
The Yellow Sea ◽  
Eastern Asia ◽  
The West ◽  
The North ◽  
Neolithic Age ◽  
Western Asia ◽  
The Neolithic Age

Northern China forms an integral part of the north temperate zone of the Old World. It is, moreover, connected with western Asia and eastern Europe by a long but continuous belt of steppe presenting no transverse barriers to migration, whether faunal or human. It cannot, therefore, be treated as a region apart, save in a very limited and subordinate sense.The surface consists in the main of mountains in the west and of plains in the east. Over much of it lie thick deposits of loess, extending from Chinese Turkistan right across eastern Asia, nearly to the Yellow Sea. These great accumulations of wind-borne soil were most probably formed during times roughly contemporary with the Riss-Wurm glaciation of Europe.

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