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Structural Geology Analysis In A Disaster-Prone Of Slope Failure, Merangin Village, Kuok District, Kampar Regency, Riau Province

机译:廖内省金宝郡库克区Merangin村斜坡失稳灾害点的结构地质分析

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The geological disaster of landslide has occurred in Merangin Village, Kuok Subdistrict, Kampar Regency, Riau Province which located exactly in the national road of Riau - West Sumatra at Km 91. Based on the occurrence of landslide, this research was conducted to study geological structure and engineering geology to determine the main factors causing landslides. Based on measurement of the structural geology found on research area, there were fractures, faults and fold rocks which having trend of stress N 2380 E, plunge 60, trending NE-SW direction. Several faults that found was normal faults directing N 2000 E with dip 200 trending from northeast-southwest and reverse fault impinging N 550 E with dip 550, pitch 200 trending to the northeast. Fold structures showing azimuth N 2010 E trending southeast-northwest. From geological engineering analysis, the results of scan line at 6 sites that have RQD value ranges 9.4% - 78.7 % with discontinuity spacing 4 - 20 cm. So, It can be concluded that the formed structure was influenced by the extensive northeast-southwest tectonic phase, then continued through north-south tectonic phase, and ended by a tectonic period with directing from northeast-southwest. Rock Mass Rating classification showing value 62 – 76, Which also resulted that rocks in the study area have weathered on the outside but still in good condition (good rock). However, This condition of structure has caused the formation rocks producing weak zone that became one cause of the occurrence of landslides.
机译:滑坡的地质灾害发生在恰好位于廖内-西苏门答腊国道91公里处的廖内省金宝郡Kuok街道Merangin村。基于滑坡的发生,本研究旨在研究地质构造和工程地质,以确定引起滑坡的主要因素。根据对研究区发现的构造地质的测量,发现有裂缝,断层和褶皱岩,其应力趋势为N 2380 E,倾角为60,方向为NE-SW。发现的几个断层是正断层,指示N 2000 E的倾角为200°,从东北-西南方向延伸;反向断层冲击N 550 E的倾角为550 N的方向,向北倾斜200度。折叠结构显示出N 2010 E方位角,向东南-西北方向发展。根据地质工程分析,在6个位置的RQD值范围为9.4%-78.7%,不连续间隔为4-20 cm,扫描线的结果。因此,可以得出这样的结论:形成的构造受东北-西南广泛的构造阶段的影响,然后一直延续到南北构造阶段,并以从东北-西南方向的构造时期结束。岩石质量等级分类显示值62-76,这也导致研究区域中的岩石已在外部风化,但仍处于良好状态(优质岩石)。但是,这种构造条件导致地层岩石产生薄弱带,这成为了发生滑坡的原因之一。

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