{"title":"侏罗纪孔隙系统的区域问题:棘皮动物、合成过度生长胶结物和第五孔隙。第九届中东地球科学会议,2010。","authors":"E. A. Clerke","doi":"10.3997/2214-4609-PDB.248.266","DOIUrl":null,"url":null,"abstract":"Regional and well-established geological and diagenetic processes are re-examined in Jurassic carbonate reservoirs using the large amount of quantitative mercury injection capillary pressure (MICP) pore system data acquired by Saudi Aramco in the last eight years. An extensive Berri Field dataset included petrographic data and MICP pore system data obtained by Thomeer analysis. The Berri data from four Jurassic carbonate reservoirs is compared to other data, and specifically the Ghawar Rosetta Stone data using a regional depositional context. The anticipated increase of Jurassic carbonate-rim cement to the north of Ghawar is evident. Much more important from a pore system perspective are the amounts of syntaxial overgrowth cement and the correlative increase of echinoderms and foraminifera in the Hadriya and Fadhili. These latter increases necessitate a fifth porositon (F-ESO), an additional maximum pore-throat diameter mode in the Hadriya and Fadhili pore system models, as compared to the four porositions that describe the pore systems of the Ghawar Arab D limestone and the Berri Arab and Hanifa reservoirs. Review of the Abqaiq Field petrographic and MICP data of Ross et al. (1995) provide independent support for the four porositons of Clerke et al. (2008) and also indicate the presence of a fifth (F-ESO) porositon in the Abqaiq Arab D. \n\nThe pore system effect of the predicted and present carbonate rim cements is imperceptible. Echinoderm and foraminifera are very abundant in the Berri Fadhili and show a steady decrease in abundance upward through the Berri Jurassic section, that is, the Fadhili, Hadriya, Hanifa and the Arab. Echinoderm abundance is closely linked to marine salinities and high magnesium calcite. Quantitative determinations of echinoderm and foraminifera abundance are shown to be correlative to and useful as a predictor of the pore destructive syntaxial overgrowth cement. Regional models of reservoir quality distribution could potentially be improved using maps of high precision Ca/Mg ratio relating to the high magnesium calcite of echinoderms and syntaxial overgrowth cements and maps of echinoderm abundances and habitats. These regional maps could relate broadly and inversely to reservoir quality and depositional salinity.","PeriodicalId":275861,"journal":{"name":"GeoArabia, Journal of the Middle East Petroleum Geosciences","volume":"249 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2010-03-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Regional issues in Jurassic pore systems: Echinoderms, syntaxial overgrowth cements and a fifth porositon. 9th Middle East Geosciences Conference, GEO 2010.\",\"authors\":\"E. A. Clerke\",\"doi\":\"10.3997/2214-4609-PDB.248.266\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Regional and well-established geological and diagenetic processes are re-examined in Jurassic carbonate reservoirs using the large amount of quantitative mercury injection capillary pressure (MICP) pore system data acquired by Saudi Aramco in the last eight years. An extensive Berri Field dataset included petrographic data and MICP pore system data obtained by Thomeer analysis. The Berri data from four Jurassic carbonate reservoirs is compared to other data, and specifically the Ghawar Rosetta Stone data using a regional depositional context. The anticipated increase of Jurassic carbonate-rim cement to the north of Ghawar is evident. Much more important from a pore system perspective are the amounts of syntaxial overgrowth cement and the correlative increase of echinoderms and foraminifera in the Hadriya and Fadhili. These latter increases necessitate a fifth porositon (F-ESO), an additional maximum pore-throat diameter mode in the Hadriya and Fadhili pore system models, as compared to the four porositions that describe the pore systems of the Ghawar Arab D limestone and the Berri Arab and Hanifa reservoirs. Review of the Abqaiq Field petrographic and MICP data of Ross et al. (1995) provide independent support for the four porositons of Clerke et al. (2008) and also indicate the presence of a fifth (F-ESO) porositon in the Abqaiq Arab D. \\n\\nThe pore system effect of the predicted and present carbonate rim cements is imperceptible. Echinoderm and foraminifera are very abundant in the Berri Fadhili and show a steady decrease in abundance upward through the Berri Jurassic section, that is, the Fadhili, Hadriya, Hanifa and the Arab. Echinoderm abundance is closely linked to marine salinities and high magnesium calcite. Quantitative determinations of echinoderm and foraminifera abundance are shown to be correlative to and useful as a predictor of the pore destructive syntaxial overgrowth cement. Regional models of reservoir quality distribution could potentially be improved using maps of high precision Ca/Mg ratio relating to the high magnesium calcite of echinoderms and syntaxial overgrowth cements and maps of echinoderm abundances and habitats. 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引用次数: 0
摘要
利用沙特阿美公司在过去8年中获得的大量定量压汞毛细管压力(MICP)孔隙系统数据,对侏罗系碳酸盐岩储层中区域和成熟的地质和成岩过程进行了重新研究。广泛的Berri油田数据集包括岩石学数据和通过Thomeer分析获得的MICP孔隙系统数据。Berri的4个侏罗系碳酸盐岩储层数据与其他数据进行了比较,特别是与Ghawar Rosetta Stone的区域沉积背景数据进行了比较。加瓦尔北部侏罗系碳酸盐岩胶结物的预期增加是明显的。从孔隙系统的角度来看,更重要的是Hadriya和Fadhili的合成过度生长胶结物的数量以及相关的棘皮动物和有孔虫的增加。与Ghawar Arab D灰岩、Berri Arab和Hanifa储层孔隙系统的4个孔隙相比,后者的增加需要第5个孔隙(F-ESO),这是Hadriya和Fadhili孔隙系统模型中额外的最大孔喉直径模型。对Abqaiq油田岩石学和Ross等人(1995)的MICP数据的回顾为Clerke等人(2008)的四个孔隙提供了独立的支持,并表明在Abqaiq阿拉伯d区存在第五个(F-ESO)孔隙。预测的和现在的碳酸盐胶结物的孔隙系统效应是不可察觉的。棘皮动物和有孔虫在Berri Fadhili非常丰富,并在Berri侏罗纪剖面(即Fadhili, Hadriya, Hanifa和Arab)中呈下降趋势。棘皮动物的丰度与海洋盐度和高镁方解石密切相关。棘皮动物和有孔虫丰度的定量测定被证明与孔隙破坏性合成过度生长胶结相关且有用。利用与棘皮动物高镁方解石和合生过生胶结物相关的高精度Ca/Mg比值图以及棘皮动物丰度和栖息地图,可以改进储层质量分布的区域模型。这些区域图可能与储层质量和沉积盐度有广泛和相反的关系。
Regional issues in Jurassic pore systems: Echinoderms, syntaxial overgrowth cements and a fifth porositon. 9th Middle East Geosciences Conference, GEO 2010.
Regional and well-established geological and diagenetic processes are re-examined in Jurassic carbonate reservoirs using the large amount of quantitative mercury injection capillary pressure (MICP) pore system data acquired by Saudi Aramco in the last eight years. An extensive Berri Field dataset included petrographic data and MICP pore system data obtained by Thomeer analysis. The Berri data from four Jurassic carbonate reservoirs is compared to other data, and specifically the Ghawar Rosetta Stone data using a regional depositional context. The anticipated increase of Jurassic carbonate-rim cement to the north of Ghawar is evident. Much more important from a pore system perspective are the amounts of syntaxial overgrowth cement and the correlative increase of echinoderms and foraminifera in the Hadriya and Fadhili. These latter increases necessitate a fifth porositon (F-ESO), an additional maximum pore-throat diameter mode in the Hadriya and Fadhili pore system models, as compared to the four porositions that describe the pore systems of the Ghawar Arab D limestone and the Berri Arab and Hanifa reservoirs. Review of the Abqaiq Field petrographic and MICP data of Ross et al. (1995) provide independent support for the four porositons of Clerke et al. (2008) and also indicate the presence of a fifth (F-ESO) porositon in the Abqaiq Arab D.
The pore system effect of the predicted and present carbonate rim cements is imperceptible. Echinoderm and foraminifera are very abundant in the Berri Fadhili and show a steady decrease in abundance upward through the Berri Jurassic section, that is, the Fadhili, Hadriya, Hanifa and the Arab. Echinoderm abundance is closely linked to marine salinities and high magnesium calcite. Quantitative determinations of echinoderm and foraminifera abundance are shown to be correlative to and useful as a predictor of the pore destructive syntaxial overgrowth cement. Regional models of reservoir quality distribution could potentially be improved using maps of high precision Ca/Mg ratio relating to the high magnesium calcite of echinoderms and syntaxial overgrowth cements and maps of echinoderm abundances and habitats. These regional maps could relate broadly and inversely to reservoir quality and depositional salinity.