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:岩石物理和仿古方面对埃及西奈北埃博伊尔·清醒的白云岩序列的地质力学性质的影响

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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:本文的目的是证明矿物质组合物,成岩病史和岩石物理性质对北西奈州型截面的地质力学性能和耐久性的控制效应及其经济潜力施工目的。岩体研究包括矿物质组合物和成岩工艺的描述,而岩石物理学研究会测量密度,孔隙率,渗透率和真正的形成电阻率因子。此外,进行了一些地质力学实验室测试,包括矿物质组合物的岩体描述和成岩数,以及施密锤数(SHV),点载荷指数(IS50),单轴抗压强度(UCS)和超声波纵向波速度测量。扫描电子显微镜用于帮助孔型描述(晶间,vuggy等)。基于岩性变化和矿物质组合物,el-卤素形成可以细分为三个非正式成员:(1)低摩尔石灰石,(2)中含有含有含沙岩岩甾酮和(3)上层司机成员。岩化性地,序列由三种显性微缩放量组成:(1)白云岩泥岩微缩醛(二孔岩微型胶质剂),(2)Dolowackestone(粘土到含有桑迪二核霉素),和(3)Dolomudstone Microfacies(Dolosparite)。最多诊断的成岩工艺是辅导,通过方解石的胶结,引起的新立参和创建神义的核心。在研究领域,多元化率几乎影响了所有的临床演替。 SHV,IS50和样品的UCS值表示高强度岩石。本研究表明了地质力学性质对岩石物理性质和研究岩石的矿物成分的依赖性。建模该性质表明可以应用于预测和表征其他地方的白云岩EL-HANAL形成之间的不同参数之间的可靠相关性。本研究的结果对于研究类似的白云岩序列的地质力学和岩石物理性质以及将其作为建筑材料的潜力排名。

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