Proceedings of the 2016 4th International Conference on Machinery, Materials and Computing Technology

Main constructive diagenesis of middle-lower Ordovician of Yubei Area in Tarim Basin

Authors
Hanting Zhao, Tailiang Fan
Corresponding Author
Hanting Zhao
Available Online March 2016.
DOI
https://doi.org/10.2991/icmmct-16.2016.184How to use a DOI?
Keywords
Yubei area;Tarim;Ordovician;Diagenesisï¼›
Abstract
According to analysis of cores, rock sections, casting sections, logging data of Ordovician carbonate reservoirs in the Yubei area,reservoir rock in the study area include 4 types:mud micrite limestone,grain limestone,biological limestone and dolomitic limestone.In combination with core photos and imaging logging analysis,reservoir can be divided into pores and cracks.Diagenesis mainly includes compaction, pressolution, cementation, filling, recrystallization, dolomitization, dissolution .To sum up, the main constructive diagenesis include recrystallization, dolomitization, dissolution,otherwise the main destructive diagenesis include compaction, pressolution, cementation, filling.
Open Access
This is an open access article distributed under the CC BY-NC license.

Download article (PDF)

Volume Title
Proceedings of the 2016 4th International Conference on Machinery, Materials and Computing Technology
Series
Advances in Engineering Research
Publication Date
March 2016
ISBN
978-94-6252-165-0
ISSN
2352-5401
DOI
https://doi.org/10.2991/icmmct-16.2016.184How to use a DOI?
Open Access
This is an open access article distributed under the CC BY-NC license.

Cite this article

TY  - CONF
AU  - Hanting Zhao
AU  - Tailiang Fan
PY  - 2016/03
DA  - 2016/03
TI  - Main constructive diagenesis of middle-lower Ordovician of Yubei Area in Tarim Basin
BT  - Proceedings of the 2016 4th International Conference on Machinery, Materials and Computing Technology
PB  - Atlantis Press
SP  - 924
EP  - 928
SN  - 2352-5401
UR  - https://doi.org/10.2991/icmmct-16.2016.184
DO  - https://doi.org/10.2991/icmmct-16.2016.184
ID  - Zhao2016/03
ER  -