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Determination of Key Beds from the Cap Rocks of Oil Reservoirs Using a Novel Method, Case Study: The Gachsaran Formation, Southwest Iran
Lithology and Mineral Resources ( IF 0.8 ) Pub Date : 2021-11-17 , DOI: 10.1134/s0024490221060055
Saeid Pourmorad 1 , Amir Jokar 2 , Shakura Jahan 3
Affiliation  

Abstract

The use of key beds in the cap rocks of the oil reservoirs is crucial. Lack of awareness of these key beds will have serious risks and damages. The Gachsaran oil field is located 220 km southwest of Ahwaz-Iran. The former caprock consists of six key beds (A, B, C, D, E, and F). At the time of writing this paper these key beds are being used during excavations and drilling to determine the site of casing points. What has made utilizing these key beds during excavations difficult however, is use of diamond drill bits which results in the shattering of excavated samples. As such, it has become challenging to learn more about these key beds through studying petrographic thin sections in microscopy. These key beds were observed during the investigation at the drill sites. Later, the excavated samples were studied in the Energy-Dispersive X-ray Spectroscopy (EDS) machine, using a semi-quantitative method to analyze the elemental differences in those key beds. In addition to the identification of various lithological and diagenetic properties of the caprock, this study leads to the introduction of four new key beds based on geochemical properties. Some of the most important differences within the formation include those between the caprock anhydrite and the non-caprock anhydrite, namely the presence of potassium and titanium and the absence of chlorine and sodium in the caprock section. The four new key beds introduced from this study using elemental differences were named as key beds-1, 2, 3, and 4.



中文翻译:

使用新方法确定油藏盖层关键层,案例研究:伊朗西南部 Gachsaran 地层

摘要

在油藏盖层中使用关键层是至关重要的。缺乏对这些重点病床的认识将带来严重的风险和损害。Gachsaran 油田位于伊朗阿瓦士西南 220 公里处。前盖层由六个关键层(A、B、C、D、E 和 F)组成。在撰写本文时,这些关键层正被用于挖掘和钻井过程中,以确定套管点的位置。然而,在挖掘过程中使用这些键床变得困难的是,使用金刚石钻头会导致挖掘出的样品破碎。因此,通过在显微镜下研究岩相薄片来了解更多关于这些关键层的信息变得具有挑战性。在钻探现场进行调查期间观察到了这些关键层。之后,在能量色散 X 射线光谱 (EDS) 机器中研究挖掘出的样品,使用半定量方法分析这些关键层中的元素差异。除了识别盖层的各种岩性和成岩特性外,本研究还根据地球化学特性引入了四个新的关键层。地层中一些最重要的差异包括盖层硬石膏和非盖层硬石膏之间的差异,即在盖层部分存在钾和钛以及不存在氯和钠。本研究中使用元素差异引入的四个新关键床被命名为关键床 1、2、3 和 4。除了识别盖层的各种岩性和成岩特性外,本研究还根据地球化学特性引入了四个新的关键层。地层中一些最重要的差异包括盖层硬石膏和非盖层硬石膏之间的差异,即在盖层部分存在钾和钛以及不存在氯和钠。本研究中使用元素差异引入的四个新关键床被命名为关键床 1、2、3 和 4。除了识别盖层的各种岩性和成岩特性外,本研究还根据地球化学特性引入了四个新的关键层。地层中一些最重要的差异包括盖层硬石膏和非盖层硬石膏之间的差异,即在盖层部分存在钾和钛以及不存在氯和钠。本研究中使用元素差异引入的四个新关键床被命名为关键床 1、2、3 和 4。即在盖层部分存在钾和钛,而没有氯和钠。本研究中使用元素差异引入的四个新关键床被命名为关键床 1、2、3 和 4。即在盖层部分存在钾和钛,而没有氯和钠。本研究中使用元素差异引入的四个新关键床被命名为关键床 1、2、3 和 4。

更新日期:2021-11-17
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