el Kohol地区(阿尔及利亚撒哈拉中部阿特拉斯)的压裂和变形带:分形分析、尺度定律和离散裂缝网络模型

IF 0.8 4区 地球科学 Q3 GEOLOGY
Réda Samy Zazoun, A. Marok, L. Samar, M. Benadla, H. Mezlah
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引用次数: 2

摘要

本文的目的是研究位于阿尔及利亚撒哈拉沙漠中部Djebel Amour的El Kohol构造的天然裂缝和变形带。野外观测和测量分别在结构前肢和后肢的两个位置进行。露头研究表明存在5个断裂组和3个变形带组。不同裂缝组的间距和长度分布模型服从幂律。整个地层的力学层厚分析表明,存在12个具有层控作用的力学单元。变形带在靠近主要断裂时,数量增加,间距减小。断裂、裂缝及变形带的分形分析呈现二维分形特征。通过将离散裂缝网络(DFN)模型计算的密度和强度参数(Pxy)与露头的密度和强度参数(Pxy)进行比较,得到了较好的相关系数。讨论了该模型与该地区识别的变形事件的关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
La fracturation et les bandes de déformation dans la région d’El Kohol (Atlas saharien central, Algérie): analyse fractale, lois d’échelles et modèle de réseaux de fractures discrètes
The aim of this paper is focused on the study of natural fractures and deformation bands in El Kohol structure, located in the Djebel Amour in the Central Saharan Atlas, Algeria. The field observations and measurements were performed through two localities on the forelimb and two others on the backlimb of the structure. The outcrop study has shown the existence of five fracture sets and three deformation bands sets. The spacing and length distribution models of the different fractures sets obey to a power law. The mechanical layer thickness analysis for the whole formations shows the existence of twelve mechanical units with a stratabound control. The deformation bands show an increasing in their numbers, and a decreasing in their spacing when they approach the major faults. The fractal analysis of faults and fractures, as well as the deformation bands show a fractal character of 2D dimension. A good correlation coefficients is obtained from the comparison between the density and the intensity parameters (Pxy) calculated from the discrete fracture network (DFN) modelling, and those from the outcrops. The model developed is discussed related to deformation events recognized in the area.
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来源期刊
CiteScore
1.40
自引率
14.30%
发文量
6
审稿时长
>12 weeks
期刊介绍: Since 1945 Estudios Geologicos publishes original research works, as well as reviews, about any topic on Earth Sciences. Estudios Geologicos is published as one yearly volume, divided into two half-yearly issues. It is edited by the Spanish National Research Council (Consejo Superior de Investigaciones Científicas, CSIC) at the Instituto de Geociencias (CSIC-UCM). Estudios Geologicos provides free access to full-text articles through this electronic edition. Accepted articles appear online as "Forthcoming articles" as soon as the galley proofs have been approved by the authors and the Editor-in-Chief. No changes can be made after online publication.
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