PENENTUAN LITOLOGI LAPISAN BAWAH PERMUKAAN BERDASARKAN TOMOGRAFI SEISMIK REFRAKSI UNTUK GEOTEKNIK BENDUNGAN AIR DAERAH “X”

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I3.1074
Hilman Sabiq, Syamsurijal Rasimeng, Karyanto Karyanto
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引用次数: 1

Abstract

Batang Toru river which is through Kecamatan Sipirok, Kabupaten Tapanuli Selatan, will be a hydro-electric power plant, in order to require the electricity in North Sumatera area. Therefore, refraction seismic survey needed to determine the subsurface litology, as a guide in the construction of river water dam in that area. This study aims to determine lithology in the research area based on cross-section of refraction seismic tomography, and to estimate the depth and thickness of the rock layers beneath the surface of the study area. Refraction seismic tomography produces a cross section which shows the distribution of velocity value to depth, so we obtain the interpretation of rock lithology and depth estimation of each layer. The first layer is a topsoil layer with a velocity range of 100-700 m/s, the thickness of the topsoil is estimated to be about 1-10 meters. The second layer is indicated as a tuff-sandstone with medium consolidation with a velocity range of 600-1800 m/s, with an estimated thickness about 10-35 meters. The third layer is indicated as a tuff-sand rock to tuff-breccia with a value range higher than 1800 m/s, with an estimated depth of 30-40 meters from the surface.
基于“X”的地质空气断层模拟折射的岩性发展
Batang Toru河穿过Kecamatan Sipirok,Kabupaten Tapanuli Selatan,将成为一座水力发电厂,以满足北苏门答腊地区的电力需求。因此,折射地震勘探需要确定地下岩性,以指导该地区的河水坝建设。本研究旨在根据折射地震层析成像剖面确定研究区的岩性,并估计研究区地表下岩层的深度和厚度。折射地震层析成像产生一个横截面,显示速度值随深度的分布,从而获得岩石岩性的解释和各层的深度估计。第一层是速度范围为100-700m/s的表层土,表层土的厚度估计约为1-10米。第二层为凝灰岩砂岩,中等固结,速度范围为600-1800 m/s,估计厚度约10-35米。第三层为凝灰岩砂岩至凝灰岩角砾岩,其数值范围高于1800 m/s,估计距离地表的深度为30-40米。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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JGE
JGE
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22 weeks
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