Lithology Identification Through X-Ray Fluorescence (XRF) Analyses on Drill Cuttings While Drilling in Santos Basin

Filipe Vidal C. S. R. Soares de Oliveira, Ricardo Tepedino Martins Gomes, Carlos Eduardo Dias Roriz, Krishna Milani Simões Silva, Rafael Correa de Toledo
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Abstract

The present research propouses a methodology using XRF analysis on drill cuttings samples, obtained during well drilling, for characterizing pre-salt reservoir formations in the Santos Basin, southeast of Brazil in order to identify composition variations in carbonates, clay zones and potential igneous rocks. In this study 16 off-set wells were analyzed where XRF analysis was performed on drill cuttings samples. Aftwerwards the results were compared with lithogeochemical and gamma-ray spectral logs, determining the consistency of the data. The lithological interpretations were based on macroscopic (sidewall core samples - SWC) and microscopic (thin section) descriptions and geochemical analyses from SWC samples. This permitted us to comprehend the variations observed in the carbonate reservoir and to identify possible igneous rocks. From the results, a pattern of responses could be established for the XRF method for each lithology within the Pre-salt section, using the major elements (Mg, Ca, Si, k, Fe and Al) and some minor elements and trace elements (Sr, Rb, Y, Zr, Ti, Nb, Ga). The variations of the major elements were best observed in radar and bar charts, that use only the major elements, which enabled the separation of the lithological section into six main sets: limestones, dolomitic carbonates, silicified carbonates, carbonates with magnesian clay, siliciclastic rocks (shale/siltstone/sandstone) and basic igneous rocks (basalt/diabase). For quality control, still during drilling, comparative analysis by three approaches was proposed: a) the systematic comparison of the proportion of elements composing the same mineral, such as Ca and Sr, K and Rb, and Al and Ga; b) the comparison of XRF data with XRD data; and c) comparison with calcimetry data in a cutting sample. Furthermore, in order to support the interpretations, four crossplots (Ca × Si; K.Rb × Al.Zr; Rb × Sr; Zr × Fe) and one crossover (Rb × Sr) were generated aiming to individualize the six lithological types described, as well as diagrams from the literature to identify the igneous rock type. The use of XRF on cuttings to determine lithologies during the drilling of petroleum wells is new in the literature, as well as the proposed quality control, being useful for the characterization of complex reservoirs such as Santos Basin pre-salt, being a methodology already used since 2018 by Petrobras.
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桑托斯盆地钻井岩屑的x射线荧光(XRF)岩性鉴定
本研究提出了一种利用XRF分析钻井过程中获得的钻屑样品的方法,用于表征巴西东南部桑托斯盆地盐下储层,以识别碳酸盐岩、粘土带和潜在火成岩的组成变化。在这项研究中,对16口井进行了XRF分析,并对钻屑样品进行了分析。然后将结果与岩石地球化学和伽马能谱测井进行比较,确定数据的一致性。岩石学解释基于宏观(侧壁岩心样品- SWC)和微观(薄片)描述以及SWC样品的地球化学分析。这使我们能够理解在碳酸盐岩储层中观察到的变化,并确定可能的火成岩。结果表明,利用主元素(Mg、Ca、Si、k、Fe和Al)和少量元素和微量元素(Sr、Rb、Y、Zr、Ti、Nb、Ga),可以建立盐下剖面各岩性的XRF方法响应模式。主要元素的变化在雷达和柱状图中得到了最好的观察,它们只使用主要元素,这使得岩性剖面分为六个主要组:石灰石、白云岩碳酸盐、硅化碳酸盐、含镁粘土的碳酸盐、硅屑岩(页岩/粉砂岩/砂岩)和基性火成岩(玄武岩/辉绿岩)。为了控制质量,在钻孔过程中,提出了三种对比分析方法:a)系统比较构成同一矿物的Ca和Sr、K和Rb、Al和Ga等元素的比例;b) XRF数据与XRD数据的比较;c)与切割样品中钙量测定数据的比较。此外,为了支持这些解释,采用了四个交叉图(Ca × Si;王立强;Rb × Sr;Zr × Fe)和一个交叉(Rb × Sr)旨在对描述的6种岩性类型进行个性化,并从文献中生成图以识别火成岩类型。在油井钻探过程中,对岩屑使用XRF来确定岩性在文献中是新的,以及所提出的质量控制,对于桑托斯盆地盐下等复杂储层的表征是有用的,这是巴西国家石油公司自2018年以来已经使用的一种方法。
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