巴基斯坦盐和跨印度河山脉下侏罗统碎屑沉积岩的沉积学和储层特征:来自岩石学、扫描电镜和岩石物理学的证据

IF 1.9 3区 地球科学 Q1 GEOLOGY
Salman Ahmed Khattak, Nasar Khan, Waseem Khan, S. Sahaya Jude Dhas, George Kontakiotis, Ihtisham Islam, Hammad Tariq Janjuhah, Assimina Antonarakou
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引用次数: 0

摘要

本文利用岩石学、扫描电镜和岩石物理分析等方法,研究了下侏罗统盐系和印度河流域下侏罗统砂岩的组成、成岩作用、物源和储层性质。达塔组碎屑矿物组成表明,砂岩类型为石英、岩屑-石英、岩屑-长石-石英、岩屑-石英-长石、石英-岩屑和长石-石英,主要来自马拉尼火成岩套、Aravali Range和Nagar Parkar等再造造山带。Datta组的颗粒由亚角到圆角,细到粗,中等到分选良好。许多发生在成岩作用早期到晚期的诊断过程,如压实作用、压力溶解作用、胶结作用、蚀变作用、白云石化作用和溶蚀作用,都得到了Datta组证据的支持。溶蚀作用、物理压实作用、白云化作用和蚀变作用提高了储层质量,而压力溶解作用和胶结作用降低了达塔组储层质量。扫描电镜下达达组孔隙类型为孔洞型、晶内/粒内型、溶蚀型和晶间型,平均岩石视觉孔隙度为11%。Chonai-01井达塔组岩石物理特征及4口井对比表明,油气向Isa-Khail-01井方向上移,沉积厚度较大,建议钻探。通过与特提斯东部其他地区Datta组年龄相当单元的比较,可以更好地了解储层非均质性,为今后具有类似地质条件的地区进行石油勘探提供依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Sedimentology and reservoir characterisation of Lower Jurassic clastic sedimentary rocks, Salt and Trans Indus Ranges, Pakistan: Evidence from petrography, scanning electron microscopy and petrophysics

Sedimentology and reservoir characterisation of Lower Jurassic clastic sedimentary rocks, Salt and Trans Indus Ranges, Pakistan: Evidence from petrography, scanning electron microscopy and petrophysics

In this study, sandstones of the Lower Jurassic Datta Formation in the Salt and Trans-Indus ranges are investigated regarding composition, diagenesis, provenance and reservoir properties using petrography, scanning electron microscopy and petrophysical analysis. The detrital mineral composition of the Datta Formation indicated that the sandstones are quartzose, lithic-quartzose, lithic-feldspatho-quartzose, lithic-quartzo-feldspathic, quartzo-lithic and feldspatho-quartzose, primarily from the recycled orogen setting, including the Malani Igneous Suite, the Aravali Range and Nagar Parkar. The Datta Formation has sub-angular to well-rounded, fine to coarse and moderate to well-sorted grains. Numerous diagnostic processes that occurred in the early to late stages of diagenesis, such as compaction, pressure solution, cementation, alteration, dolomitisation and dissolution, are supported by evidence in the Datta Formation. Dissolution, physical compaction, dolomitisation and alteration enhanced the reservoir quality, while pressure solution and cementation reduced the reservoir quality of the Datta Formation. The porosity types detected in the Datta Formation under scanning electron microscopy are vuggy, intracrystalline/intraparticle, dissolution and intercrystalline, with an average petrographic visual porosity of 11%. The petrophysical aspects of the Datta Formation in the Chonai-01 well and the correlation between four wells indicated that the hydrocarbons had shifted up-dip towards the Isa-Khail-01 well, so it is recommended for drilling because of the greater depositional thickness. The comparison of the Datta Formation with age-equivalent units in other regions of eastern Tethys provided a better understanding of reservoir heterogeneities that can be applicable in areas with similar geological conditions for future petroleum exploration.

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来源期刊
CiteScore
4.10
自引率
16.70%
发文量
42
审稿时长
16 weeks
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