DocumentCode
1897698
Title
Notice of Retraction
Subsidence History Simulation and Its Application in Paleogene of Qiongdongnan Basin
Author
Jun Xiao ; Bei Zhu
Author_Institution
Fac. of Earth Resources, China Univ. of Geosci., Wuhan, China
fYear
2010
fDate
25-26 Dec. 2010
Firstpage
1
Lastpage
4
Abstract
Notice of Retraction
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
Subsidence history simulation is useful tool for sedimentary basin analysis, and backstripping is the most important method. In this study, taking Qiongdongnan basin as an example, the Paleocene subsidence characteristics are analyzed. This basin is characterized by episodic subsidence, but the difference is gradually reducing with geological time. The subsidence centers are migratory. The sags in central depression zone are the main subsidence areas with higher subsidence values, and other sags in northern or southern depression zones are the secondary subsidence areas with lower subsidence values.
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
Subsidence history simulation is useful tool for sedimentary basin analysis, and backstripping is the most important method. In this study, taking Qiongdongnan basin as an example, the Paleocene subsidence characteristics are analyzed. This basin is characterized by episodic subsidence, but the difference is gradually reducing with geological time. The subsidence centers are migratory. The sags in central depression zone are the main subsidence areas with higher subsidence values, and other sags in northern or southern depression zones are the secondary subsidence areas with lower subsidence values.
Keywords
geochronology; geomorphology; geophysical techniques; palaeontology; sediments; China; Paleocene subsidence characteristics; Qiongdongnan basin Paleogene; backstripping; central depression zone; episodic subsidence; sedimentary basin analysis; subsidence center; subsidence history simulation; Analytical models; Compaction; Geology; History; Laboratories; Load modeling; Sediments;
fLanguage
English
Publisher
ieee
Conference_Titel
Information Engineering and Computer Science (ICIECS), 2010 2nd International Conference on
Conference_Location
Wuhan
ISSN
2156-7379
Print_ISBN
978-1-4244-7939-9
Type
conf
DOI
10.1109/ICIECS.2010.5678201
Filename
5678201
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