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首页> 外文期刊>Fresenius environmental bulletin >STUDY ON THE SEQUENCE DIVISION AND RESERVOIR OF MIDDLE PERMIAN IN CENTRAL SICHUAN BASIN, CHINA
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STUDY ON THE SEQUENCE DIVISION AND RESERVOIR OF MIDDLE PERMIAN IN CENTRAL SICHUAN BASIN, CHINA

机译:四川盆地中部中二叠统层序划分与储层研究

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摘要

Carbonate reservoirs are developed in Qixia and Maokou Formations of Middle Permian in central Sichuan. In this paper, the sequence of the study area is divided according to the core and logging data, and the reservoir characteristics are also studied. The results show that (i) Qixia Formation can be divided into one third order sequence and Maokou Formation can be divided into two third-order sequences. Each third order sequence can be subdivided into two system tracts, transgression system tract (TST) and highstand system tract (HST); (ii) Reservoirs in the study area mainly include dolomite, bioclastic limestone and fine crystalline limestone. Reservoir space types can be divided into pores, caves and fractures. The study area develops low porosity and low permeability reservoir; (iii)The porosity of Qixia Formation reservoir is mainly between 2% and 4%, the permeability is mainly between 0.1mD and 1 mD, the porosity of Maokou Formation reservoir is mainly between 0 and 2%, and the permeability is mainly between 0.1 and 1 mD.
机译:四川中部二叠系栖霞和茅口组发育碳酸盐岩储层。本文根据岩心和测井资料对研究区的层序进行了划分,并对储层特征进行了研究。结果表明:(i)栖霞组可分为一个三阶层序,茅口组可分为两个三阶层序。每个三阶序列可以细分为两个系统域:海侵系统域(TST)和高位系统域(HST); (ii)研究区的储层主要包括白云岩,生物碎屑灰岩和细晶灰岩。储层空间类型可分为孔隙,溶洞和裂缝。研究区开发了低孔低渗储层。 (iii)栖霞组储层孔隙度主要在2%至4%之间,渗透率主要在0.1mD至1mD之间,茅口组储层孔隙度主要在0%至2%之间,渗透率主要在0.1%之间和1 mD。

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