首页> 外文期刊>Bulletin of engineering geology and the environment >Impacts of the petrophysical and diagenetic aspects on the geomechanical properties of the dolomitic sequence of Gebel El-Halal, Sinai, Egypt
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Impacts of the petrophysical and diagenetic aspects on the geomechanical properties of the dolomitic sequence of Gebel El-Halal, Sinai, Egypt

机译:岩石和成岩作用对埃及西奈半岛Gebel El-Halal白云岩层序的地球力学性质的影响

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The aim of this paper is to demonstrate the controlling effect of the mineral composition, the diagenetic history and the petrophysical properties on the geomechanical properties and durability of the dolomitic El-Halal Formation in its type section in North Sinai as well as its economic potential for construction purposes. The petrographic studies include descriptions of both the mineral composition and diagenetic processes, while the petrophysical studies measure the density, porosity, permeability and true formation resistivity factor. In addition, some geomechanical laboratory tests were conducted, including the petrographic description of the mineral composition and diagenetic processes, as well as the Schmidt Hammer number (SHV), point load index (IS50), uniaxial compressive strength (UCS), and ultrasonic longitudinal wave velocity measurements. Scanning electron microscopy was used to help in pore-type description (intergranular, vuggy, etc.). Based on lithologic changes and mineral composition, the El-Halal Formation can be subdivided into three informal members: (1) lower dolomitic limestone, (2) middle sandy dolostone and (3) upper dolostone member. Petrographically, the sequence consists of three dominant microfacies: (1) dolomitic mudstone microfacies (dolomitic micrite to dolomicrite), (2) dolowackestone (clayey to sandy dolomicrite), and (3) dolomudstone microfacies (dolosparite). The most diagnostic diagenetic processes are dolomitization, cementation by calcite, aggrading neomorphism and the creation of authigenic illite. In the study area, dolomitization has affected almost all the Cenomanian succession. The SHV, IS50, and UCS values of the samples indicate high-strength rocks. The present study indicates the dependence of the geomechanical properties on the petrophysical properties and the mineral composition of the studied rocks. Modeling the properties indicates a reliable correlation between the different parameters which can be applied for predicting and characterizing the dolomitic El-Halal Formation elsewhere. The results of the present investigation are useful for studying the geomechanical and petrophysical properties of similar dolomitic sequences and in ranking its potential as construction materials.
机译:本文的目的是证明北西奈白云岩El-Halal组类型段中矿物成分,成岩史和岩石物理特性对其地质力学特性和持久性的控制作用以及其经济潜力。施工目的。岩石学研究包括矿物成分和成岩过程的描述,而岩石物理研究则测量密度,孔隙率,渗透率和真实地层电阻率因子。此外,还进行了一些地质力学实验室测试,包括矿物组成和成岩过程的岩石学描述,以及施密特锤数(SHV),点载荷指数(IS50),单轴抗压强度(UCS)和超声纵向波速测量。扫描电子显微镜用于帮助描述孔类型(晶间,松散性等)。根据岩性变化和矿物组成,可将El-Halal组划分为三个非正式成员:(1)下白云质石灰石,(2)中砂质白云岩和(3)上白云岩。岩石学上,该层序由三个主要的微相组成:(1)白云质泥岩微相(白云岩微晶岩到白云岩),(2)dolowackestone(粘土质到沙质白云岩),和(3)白云岩微相(白云岩)。诊断性最强的成岩作用是白云石化,方解石胶结,新近变质和自生伊利石的形成。在研究领域,白云石化影响了几乎所有的塞诺曼尼亚演替。样品的SHV,IS50和UCS值表示高强度岩石。本研究表明,岩石力学特性对岩石物理特性和矿物组成的依赖性。对性质进行建模表明,不同参数之间存在可靠的相关性,可将其用于预测和表征其他地方的白云质El-Halal组。本研究的结果可用于研究类似白云岩层序的地质力学和岩石物理特性,并对其作为建筑材料的潜力进行排名。

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