首页> 外文会议>Asian conference on remote sensing;ACRS >INVESTIGATION OF PALU TUNNEL DEFORMATIONS ALONG THE CREEPING SECTION (HAZAR-PALU SEGMENT) OF THE EAST ANATOLIAN FAULT, TURKEY BY TERRESTRIAL LASER SCANNER
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INVESTIGATION OF PALU TUNNEL DEFORMATIONS ALONG THE CREEPING SECTION (HAZAR-PALU SEGMENT) OF THE EAST ANATOLIAN FAULT, TURKEY BY TERRESTRIAL LASER SCANNER

机译:土耳其东部纳塔尔断裂的蠕变部分(哈扎尔-帕卢段)沿帕卢隧道变形的地面激光扫描仪研究

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The Eastern Anatolian Fault (EAF), which forms the boundary between Anatolia and Arabian plates, is one of the most important tectonic structures in the Eastern Mediterranean region. Together with its conjugate, the North Anatolian Fault (NAF), it accommodates the westward motion of the Anatolian plate with respect to Eurasia. Although it has been associated only with small-to-moderate sized earthquakes in the instrumental period and relatively quiet compared to the North Anatolian Fault, the EAF produced devastating large (M > 7) earthquakes in the historical time. Analysis of historical seismicity suggests that a seismic gap exists between the Lake of Hazar and Bingol. referred here as to Palu seismic gap. Recently, using GPS and InSAR. we showed that the 100km-long section of the Palu segment is exhibiting aseismic creep at the surface, in contrast to the previous studies. The creep rate varies along the fault reaching, at some places, to the far field GPS-based plate velocity (i.e., 10 ± 0.3 mm/yr), implying that significant portion of the elastic strain has been released aseismically. One of the best markers of the creeping zone is Palu railway tunnel that is 4.90m wide, 5.87m high and 787m long. It cuts by EAF and the walls of the tunnel have been offset by approximately 10-20 cm since construction in the middle of the last century. In this study, surface deformation of the tunnel has been investigated using Terrestrial Laser Scanner (TLS). The measurements have been performed using FARO Focus 3D X130 on 10.09.2018 and 19.06.2019, respectively. The first TLS data has been taken as reference for registration of the second TLS measurement. The registration accuracy has been calculated as 3.02 mm. Open source Cloud Compare software has been used to define changes between two- dataset. 2.05% of calculated distances were in 1 - 2.5 cm interval. However, in some small regions, distances varying between 2.5-5 cm have been observed. In this study, effects of calculated distances on the stabilization of the structure are discussed. This study showed that the TLS technique gives promising results for monitoring of surface deformation of Palu railway tunnel.
机译:构成安那托利亚和阿拉伯板块边界的东部安那托利亚断层(EAF)是东地中海地区最重要的构造构造之一。连同其共轭物北安那托利亚断层(NAF),它适应了安那托利亚板块相对于欧亚大陆的向西运动。尽管它仅在仪器化时期与中小地震有关,并且与北安纳托利亚断裂相比相对安静,但EAF在历史时期产生了毁灭性的大(M> 7)地震。对历史地震活动的分析表明,哈扎尔湖和宾格尔之间存在地震缝隙。此处称为Palu地震缝隙。最近,使用GPS和InSAR。我们发现,与以前的研究相比,帕卢(Palu)段的100公里长部分在表面表现出抗震蠕变。蠕变速率沿断层变化,在某些地方达到基于GPS的远场板速度(即10±0.3 mm / yr),这意味着很大一部分弹性应变已通过抗震释放。爬坡带最好的标志之一是帕卢铁路隧道,该隧道宽4.90m,高5.87m,长787m。自上世纪中叶开始建造以来,电弧炉切割了它,隧道的壁已经偏移了大约10-20厘米。在这项研究中,已使用地面激光扫描仪(TLS)对隧道的表面变形进行了研究。分别在2018年9月10日和2019年6月19日使用FARO Focus 3D X130进行了测量。第一个TLS数据已作为第二个TLS测量的注册参考。对位精度已计算为3.02毫米。开源Cloud Compare软件已用于定义两个数据集之间的更改。 2.05%的计算距离在1-2.5厘米间隔内。但是,在一些小区域中,观察到的距离在2.5-5厘米之间。在这项研究中,讨论了计算出的距离对结构稳定性的影响。这项研究表明,TLS技术为帕卢铁路隧道的表面变形监测提供了有希望的结果。

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