Main diagenesis of middle-lower Ordovician of Yubei Area in Tarim Basin
Hanting Zhao, Tailiang Fan
Available Online March 2016.
- https://doi.org/10.2991/icmmct-16.2016.89How to use a DOI?
- Yubei area;Tarim;Ordovician;Diagenesisï¼›
- 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 analysisï¼Œreservoir 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.
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- 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 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 - 438 EP - 444 SN - 2352-5401 UR - https://doi.org/10.2991/icmmct-16.2016.89 DO - https://doi.org/10.2991/icmmct-16.2016.89 ID - Zhao2016/03 ER -