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首页> 外文期刊>Geomorphology >Deep-seated gravitational slope deformations controlled by the structure of flysch nappe outliers: Insights from large-scale electrical resistivity tomography survey and LiDAR mapping
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Deep-seated gravitational slope deformations controlled by the structure of flysch nappe outliers: Insights from large-scale electrical resistivity tomography survey and LiDAR mapping

机译:菲施·纳普离群点结构控制的深层重力斜坡变形:大规模电阻层析成像调查和LiDAR映射的见解

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The flysch nappe outliers represent a structural setting prone to the development of deep-seated gravitational slope deformations (DSGSDs). The study area of the Palkovicke hfirky hills represents an isolated outlier of the Carpathians flysch nappes, Czech Republic. Geomorphological mapping based on field surveys and interpretation of LiDAR data reveals the occurrence of various types of slope deformations, including two DSGSDs. With the aim of detecting the main controlling factors of the DSGSDs, a multiapproach investigation combining surface and underground studies has been performed. Structural measurement points to a brachysynclinal structure composed of jointed and lithologically diverse strata with step-like topography. High-resolution LiDAR data suggest strong tectonic disruption caused by conjugated transtensional and en echelon tectonic faults controlling the course of slope segments, river valleys and landslide scarps. Four specific localities have been subjected to geophysical surveying. Kilometre-scale electrical resistivity tomography (ERT) profiles that have depths of penetration reaching the limits of the method (150 m) were acquired across the gravitationally deformed nappe outlier. The data show the overall structural conditions of the nappe outlier consisting of alternating lithological units affected by folds and fault zones. A local subordinate anticline within the central part of the brachysynclinal structure has controlled the origin of the most morphologically pronounced DSGSDs. Other large-scale DSGSDs related to the inherited fault system potentially affect the entire N/NW segment of the studied elevation. Data integration indicate that structural conditions, including lithological boundaries, tectonic disruption and local folding to be the main controlling factors of the DSGSDs evolution. (C) 2018 Elsevier B.V. All rights reserved.
机译:蝇状滑倒离群值代表着易于发生深部重力倾斜变形(DSGSD)的结构环境。 Palkovicke hfirky丘陵的研究区域代表了捷克共和国喀尔巴阡山脉的flysch尿布的孤立孤立点。基于野外调查和对LiDAR数据的解释的地貌制图揭示了各种类型的边坡变形的发生,包括两个DSGSD。为了检测DSGSD的主要控制因素,已进行了将地面和地下研究相结合的多方法研究。结构测量结果表明,由连接的,岩性不同的地层组成的近曲斜构造具有阶梯状的地形。高分辨率LiDAR数据表明,由共轭的张性和梯级构造断层控制斜坡段,河谷和滑坡陡坡的走向引起的强烈构造破坏。已对四个特定地点进行了地球物理调查。在重力变形的尿布异常点上获得了渗透深度达到方法极限(> 150 m)的千米级电阻率层析成像(ERT)剖面。数据显示了由褶皱和断层带影响的交替岩性单元组成的推覆异常条件的总体结构条件。近臂突结构中央部分的局部下背斜线控制了形态上最明显的DSGSD的起源。与继承的断层系统有关的其他大型DSGSD可能会影响研究海拔的整个N / NW段。数据整合表明,包括岩性边界,构造破坏和局部褶皱在内的结构条件是DSGSDs演化的主要控制因素。 (C)2018 Elsevier B.V.保留所有权利。

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