Impact of microfacies and diagenesis on the reservoir quality of Upper Devonian carbonates in Southeast Tatarstan, Volga-Ural Basin, Russia

Q1 Earth and Planetary Sciences Petroleum Research Pub Date : 2023-09-01 DOI:10.1016/j.ptlrs.2022.10.006
Ibrahem Yousef, V.P. Morozov, A.N. Kolchugin, A. Leontev
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引用次数: 1

Abstract

The results of integrated sedimentology, petrography, and petrophysical study of the Upper Devonian (Middle Famennian) Dankovo-Lebedyansky carbonates from Southeast Tatarstan of the Volga-Ural Basin revealed a variety of microfacies and diagenetic events that impacted the reservoir quality. Although our earlier study documented microfacies analysis and depositional environments, none of the studies focused on diagenesis, microfacies interaction, and their controls on the studied sediment's reservoir quality. Based on petrographic and microfacies analyses, the seven identified microfacies types are peloidal grainstone MF 1, cemented bioclastic peloidal grainstone MF 2, echinoderm-concentrated packstone MF 3, algae packstone MF 4, bioclastic wackestone MF 5, whole-fossil wackestone MF 6, and dolomite MF 7. For the investigated sediments, a gently deepening carbonate ramp depositional model with an inner, middle, and outer ramp setting is proposed. The observed diagenetic events in this study include micritization, calcite cementation (six cement types), dolomitization (six dolomite types), dissolution (fabric and non-fabric-selective dissolution), compaction, and microfracturing. The identified microfacies were classified into three distinct classes based on their petrophysical characteristics. MF 1 and MF 7 are microfacies types with the best reservoir quality. MF 3 and MF 4 are microfacies types of moderate reservoir quality. MF 2, MF 5, and MF 6 are microfacies types with poor or non-reservoir quality. Calcite cementation, micritization, and compaction are the primary diagenetic modifications responsible for porosity reduction. Moldic pores created by dissolution are a significant porosity-improving process. Porosity is locally enhanced by stylolite and microfractures. Dolomitization improved reservoir quality by creating intercrystalline and vuggy porosity. Understanding the impact of microfacies and diagenesis on reservoir quality is crucial for understanding reservoir properties in nearby fields with similar settings.

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俄罗斯伏尔加-乌拉尔盆地鞑靼斯坦东南部上泥盆系碳酸盐岩微相和成岩作用对储层质量的影响
伏尔加-乌拉尔盆地鞑靼斯坦东南部上泥盆纪(中法门期)Dankovo-Lebedyansky碳酸盐岩的沉积学、岩石学和岩石物理综合研究结果揭示了影响储层质量的各种微相和成岩事件。尽管我们早期的研究记录了微相分析和沉积环境,但没有一项研究关注成岩作用、微相相互作用及其对所研究沉积物储层质量的控制。根据岩相和微相分析,已确定的7种微相类型为:似球粒粒状灰岩MF1、胶结生物碎屑似球粒状灰岩MF2、棘皮动物富集泥粒灰岩MF3、藻类泥粒灰石MF4、生物碎屑粒砂岩MF5、全化石粒砂岩MF6和白云石MF7。对于所调查的沉积物,提出了一个具有内、中、外斜坡设置的平缓加深碳酸盐斜坡沉积模型。本研究中观察到的成岩事件包括泥晶化、方解石胶结(六种水泥类型)、白云石化(六种白云石类型)、溶解(组构和非组构选择性溶解)、压实和微破裂。已识别的微相根据其岩石物理特征分为三类。MF1和MF7是储层质量最好的微相类型。MF3和MF4为中等储层质量的微相类型。MF2、MF5和MF6是储层质量较差或非储层质量的微相类型。方解石胶结、微晶化和压实是导致孔隙度降低的主要成岩作用。溶解产生的发霉孔隙是一个显著的孔隙率改善过程。缝合岩和微裂缝局部增强了孔隙度。白云岩化通过形成晶间和溶洞孔隙度来改善储层质量。了解微相和成岩作用对储层质量的影响,对于了解具有类似环境的附近油田的储层性质至关重要。
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来源期刊
Petroleum Research
Petroleum Research Earth and Planetary Sciences-Geology
CiteScore
7.10
自引率
0.00%
发文量
90
审稿时长
35 weeks
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