Sedimentary sequence and environmental evolution in the eastern south Yellow Sea during the last deglaciation and the Holocene

被引：5
|
作者：
Li, SQ [1 ]
Li, JA [1 ]
Wang, SJ [1 ]
Yang, ZG [1 ]
机构：
[1] Minist Geol & Mineral Resources, Inst Marine Geol, Qingdao 266071, Peoples R China
来源：
CHINESE SCIENCE BULLETIN | 1998年 / 43卷 / 09期
关键词：
south Yellow Sea; sedimentary sequence; deposit of eddy; environmental evolution;
D O I：
10.1007/BF02898954
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
Northwest of Cheju Island in the eastern South Yellow Sea there is an are patch of muddy deposit which coincides with an anticlokwise eddy and thus is referred to as muddy deposit of eddy. Two drilling wells, the YSDP 102 well and the YSDP 103 well, penetrated the muddy deposit and revelated the sedimentary sequence in the sea area during the last deglaciation and the Holocene. Based on shallow seismic profiles, sedimentary features and dating data, stratigraphic units formed in the eastern South Yellow Sea, documents the path, time and process of the earliest post-glacial transgression in the South Yellow Sea are presented, the formation of the Yellow Sea warm current and its control over the Yellow Sea sedimentation are discussed, and deals with the source of the muddy deposit is dealt with.
引用
收藏
页码：757 / 761
页数：5
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