DocumentCode
527190
Title
Notice of Retraction
Study on sedimentary macrofacies of sandy group III of the first section of Qingshankou formation, QingNan region
Author
Dongju Ya ; Deyong Li
Author_Institution
Coll. of Marine Geosci., Ocean Univ. of China, Qingdao, China
Volume
3
fYear
2010
fDate
17-18 July 2010
Firstpage
617
Lastpage
619
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.
According to the core observation and analysis of logging data, in the stage of the sandy group III of the first section of Qingshankou formation, it mainly developed normal delta, which further classifies two subfacies delta front and prodelta. The delta front dominates a great part, and prodelta facies distributes a quite small proportion. Delta front facies can be divided into underwater distributary channel. distributary mouth bar, offshore sandbar, costal sand sheet, interdistributary bay and shallow lake - semi-deep lake mud. According to the distribution of sedimentary macrofacies, it can provide guidance to find favorable areas.
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.
According to the core observation and analysis of logging data, in the stage of the sandy group III of the first section of Qingshankou formation, it mainly developed normal delta, which further classifies two subfacies delta front and prodelta. The delta front dominates a great part, and prodelta facies distributes a quite small proportion. Delta front facies can be divided into underwater distributary channel. distributary mouth bar, offshore sandbar, costal sand sheet, interdistributary bay and shallow lake - semi-deep lake mud. According to the distribution of sedimentary macrofacies, it can provide guidance to find favorable areas.
Keywords
proxy records (geophysical); sediments; well logging; QingNan region; Qingshankou formation; core observation; costal sand sheet; distributary mouth bar; interdistributary bay; logging data; offshore sandbar; sandy group III; sedimentary macrofacies; semideep lake mud; shallow lake; underwater distributary channel; Biological system modeling; Qingshankou formation; delta; sandy group III; sedimentary model;
fLanguage
English
Publisher
ieee
Conference_Titel
Environmental Science and Information Application Technology (ESIAT), 2010 International Conference on
Conference_Location
Wuhan
Print_ISBN
978-1-4244-7387-8
Type
conf
DOI
10.1109/ESIAT.2010.5568455
Filename
5568455
Link To Document