Diagenesis impact on a deeply buried sandstone reservoir (Es1 Member) of the Shahejie Formation, Nanpu Sag, Bohai Bay Basin, East China

被引:8
|
作者
Kashif, M. [1 ,2 ]
Cao, Y. [1 ]
Yuan, G. [1 ]
Jian, W. [1 ]
Cheng, X. [1 ]
Sun, P. [1 ]
Hassan, S. [1 ,2 ]
机构
[1] China Univ Petr, Sch Geosci, Qingdao 266580, Peoples R China
[2] Univ Sargodha, Dept Earth Sci, Sargodha 40100, Pakistan
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
diagenesis; Shahejie Formation; quartz cement; calcite cement; dissolution; reservoir characteristics; porosity; permeability; ANOMALOUSLY HIGH-POROSITY; QUARTZ CEMENTATION; CLAY-MINERALS; MASS-TRANSFER; HYDROCARBON ACCUMULATION; MIOCENE SANDSTONES; SEDIMENTARY BASINS; DONGYING SAG; BENGAL BASIN; SURMA GROUP;
D O I
10.1080/08120099.2018.1490357
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Diagenesis has a significant impact on reservoir quality in deeply buried formations. Sandstone units of the Shahejie Formation (Es-1 Member) of Nanpu Sag, Bohai Bay Basin, East China is a typical deeply buried sandstone with large hydrocarbon accumulations. The methodology includes core observations and thin section studies, using fluorescence, scanning electron microscope (SEM), cathodoluminescence (CL), fluid inclusion and isotope and electron probing analysis as well as the numerical determination of reservoir characteristics. The sandstones consist of medium to coarse-grained, slight to moderate sorted lithic arkose and feldspathic litharenite. Porosity and permeability values range from 0.5 to 30% and 0.006 to 7000 mD, respectively. The diagenetic history reveals mixed episodes of diagenesis and deep burial followed by uplift. The main diagenetic events include compaction, cementation alteration, dissolution of unstable minerals and grain fracturing. Compaction resulted in densification and significantly reduced the primary porosity. Quartz, calcite and clay are the dominant pore-occluding cement and occur as euhedral to subhedral crystals. Alteration and dissolution of volcanic lithic fragments and pressure solution of feldspar grains were the key sources of quartz cement whereas carbonate cement is derived from an external source. Clay minerals resulted from the alteration of feldspar and volcanic lithic fragments. Porosity and permeability data predict a good inverse relationship with cementation whereas leaching of metastable grains, dissolution of cement and in some places formation of pore-lining chlorite enhanced the reservoir quality. The best reservoir is thicker sandstone bodies that are medium to coarse-grained, well-sorted sandstone with low primary ductile grains with a minor amount of calcite cement. The present study shows several diagenetic stages in the Es-1 Member, but the overall reservoir quality is preserved.
引用
收藏
页码:133 / 148
页数:16
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