土耳其Işıklar-Trabzon活动滑坡综合地球物理测量初步结果

M. Senkaya, A. E. Babacan, H. Karslı
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引用次数: 0

摘要

综合地球物理测量在确定滑坡类型、可能滑动破坏带的位置、土壤与基岩界面、含水带的确定以及横向和垂直方向的岩性变化等方面具有重要意义。本文介绍了在Trabzon省Macka地区Isiklar地区收集的地震折射层析成像(SRT)、多通道面波分析(MASW)、电阻率层析成像(ERT)和微震(HVSR)数据的初步评价结果。利用这些资料,采用规则过程和反演步骤,得到了二维纵波速度和ERT剖面、一维纵波速度深度剖面以及地面主频和H/V幅值。在初步结果的基础上,揭示了滑坡物质在水平和垂直方向上的可能分布,表明滑坡物质的厚度超过约12米。研究区主要物质由大小块状岩石组成,构造十分复杂。此外,SRT和ERT剖面显示出山谷状结构的存在,滑坡类型为崩塌-滑动组合。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Preliminary results of Integrated Geophysical Surveying in an active landslide in Işıklar-Trabzon, Turkey
Summary Integrated Geophysical Surveying has gain importance for landslide investigations, deciding the type of landslide, location of the possible sliding and failure zones, the interface between soil and bedrock, determining of water-containing zones, and lithological variation in lateral and vertical direction. This study presents preliminary results of the evaluation of seismic refraction tomography (SRT), multichannel analysis of surface wave (MASW), electrical resistivity tomography (ERT) and microtremor (HVSR) data collected in from an active landslide where is located in Isiklar locality of Macka district in Trabzon province. From these data, 2D P-wave velocity and ERT sections, 1D S-wave velocity depth profile, and the values of predominant frequency and H/V amplitude of ground were obtained by using regular processes and inversion steps. Based on preliminary results, possible distribution of landslide materials in the horizontal and vertical directions was revealed and it is shown that the landslide materials with a thickness exceeding approximately 12 meters. Dominant materials of study area are composed of large and small blocky rocks and have a very complex structure. Moreover, the SRT and ERT sections show the presence of a valley-shaped structure and that the type of landslide is a combination of collapse-sliding.
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