吉姆帕布米的显微地带划分方法

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I1.1054
Asri Wulandari, Suharno Suharno, R. Rustadi, Rahayu Robiana
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引用次数: 4

摘要

西苏门答腊省佩西西尔塞拉坦地区是易发生灾害的高风险地区之一。本研究旨在通过主频值、Vs30、PGA、放大等方法绘制出磐安地区的地震易发区,了解该地区的地面运动值。通过使用HVSR方法(水平与垂直光谱比)有望帮助区域分区。根据已做的研究,已知西苏门答腊磐安地区的主导频率值在0.6 ~ 12.07 Hz之间。对于Vs30在73.08 ~ 1449 m/s之间,放大值在0.47 ~ 6.01之间。磐安地区PGA值在0.034 ~ 0.063 g之间。根据对四个分区图的关联分析可知,地震灾害的高风险区域估计为沿海地区。这是由占主导地位的低频值和Vs30小值和高值的PGA支持的。这个区域的放大价值分为四个区域,地区放大非常高在海滩和岩石由冲积,放大的高价值的包含在几乎所有的地区Painan虽然放大介质和低Painan的小区域,本戈帕Salido的小区域,因为根据地质图的区域由两种类型的岩石是冲积和岩石Painan形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PEMETAAN MIKROZONASI DAERAH RAWAN GEMPABUMI MENGGUNAKAN METODE HVSR DAERAH PAINAN SUMATERA BARAT
Regional Painan, the distric of Pesisir Selatan, the province of west Sumatera is one of the areas with high risk disaster prone. This study aims attempts to maped the disaster prone area of the Painan region based on the dominant frequency value, Vs30, PGA and amplification and to know the value of ground movement from the area. By using the HVSR method (Horizontal to Vertical Spectra Ratio) expected to assist to zone the regions. Based on the research that has been done, it is known that the Painan area, West Sumatera, have values of dominant frequency between 0.6 to 12.07 Hz. As for the value Vs30 between 73.08 to 1449 m/s and the amplification values between 0.47 to 6.01. The PGA value for Painan region between 0.034 to 0.063 g. Based on the analysis that has been done by correlating the four zoning map, it is known that the area which has a high risk of earthquake disaster that is estimated to coastal areas. This is supported by the dominant low frequency value and the value Vs30 small and PGA of high value. The amplification value of this region is divided into four zones, areas that have amplification is very high being around the beach and composed by rock alluvial, the value of amplification of high contained in nearly all the regions Painan while amplification medium and low are the small area of Painan and the small area of Bungo Pasang Salido because based on the geological map of the area is composed of two types of rocks are alluvial and rock Painan Formations.
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JGE
JGE
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