塔里木盆地奥陶系层序地层格架及其对碳酸盐岩储集体发育的控制

doi:10.11743/ogg20050307

Abstract

Abstract:

Vertically,the Ordovician in Tarim basin can be divided into 2 supersequence groups,which can be further divided into 5 supersequences and 18 third-order sequences.Laterally,from west to east,the Ordovician deposits transit successively from platform facies to slope and basin facies,and the development of stratigraphic sequences appear to be progressive progradation resulting in the downlapping of a series of prograded sequences onto a relatively large downlapping surface.Sequence boundaries of various orders have important control on the development of Ordovician carbonate reservoirs in Tarim basin.The transient exposure caused by the third-order sequence boundaries and the synchronous diagenesis would have facilitated the modification of reef-bank facies reservoirs on the edge of the platform corresponding the large unconformities,which correspond to the sequence boundaries of higher levels might be the key factors that have controlled the development of the Ordovician carbonate karstic reservoirs in Tarim basin.

Key words: carbonate rocks, sequence stratigraphic framewok, reservoir, Ordovician, Tarim Basin

CLC Number:

TE111.3

Yu Bingsong, Chen Jianqiang, Lin Changsong. Sequence stratigraphic framework and its control on development of Ordovician carbonate reservoir in Tarim basin[J]. Oil & Gas Geology, 2005, 26(3): 305-309,316.

References

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Sequence stratigraphic framework and its control on development of Ordovician carbonate reservoir in Tarim basin

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