地震震源的重新定位方法是修改关节置换术(MJHD)来分析南部苏门答腊俯冲区

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I1.1059
Deswita Sari, Fadiah Khairina
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引用次数: 0

摘要

苏门答腊岛南部是两个构造板块印度-澳大利亚板块和欧亚板块交汇边界引起地震灾害的非常脆弱的地区。需要进行精确的震源分析,以了解该地区俯冲带等准确的构造背景。震源重新定位用于重新计算地震震源,使其更加准确。为了产生更准确的尿道下裂,采用改良的联合尿道下裂测定法(MJHD)进行尿道下裂复位。使用改进的联合次中心测定(MJHD)方法的重新定位使用IASP91波速,该波速假设内部结构是不均匀的。在这项研究中,使用了2010年1月至2016年12月期间的数据P波和S波到达时间,坐标为-3.5ºS.d-9ºLS-99ºS.d-106.5ºBT。使用MJHD的重新定位结果显示,地震震源的RMS(均方根)值在0.2 S.d-0.5之间变化。苏门答腊南部的部分有三次俯冲。明古鲁形成的俯冲带约为26.78º,楠榜俯冲带约30.225º,巽他海峡俯冲带约52.53º。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
RELOKASI HIPOSENTER GEMPABUMI MENGGUNAKAN METODE MODIFIED JOINT HYPOCENTER DETERMINATION (MJHD) UNTUK ANALISIS ZONA SUBDUKSI SUMATERA BAGIAN SELATAN
The part of south Sumatera is very vulnerable region in case of earthquake disaster caused by convergent boundary of two tectonic plates Indo-Australian Plates and Eurasian Plates. Precise hypocenter analysis is needed to understand about  the accurate tectonic setting such as subduction zone in the area. Hypocenter relocation is used to recalculate earthquake hypocenter to become more accurate. To produce a more accurate hyposenter this hyposenter relocation is done by using the method of Modified Joint Hypocenter Determination (MJHD). Relocation using the Modified Joint Hypocenter Determination (MJHD) method uses IASP91 wave velocity which assumes that the inner structures are heterogeneous. In this study, used data P-wave and S-wave  arrival time in the period January 2010 s.d December 2016 with coordinates -3.5º s.d -9º LS - 99º s.d 106.5º BT. The results of the relocation using MJHD showed a change of earthquake hypocenter shown by RMS (Root Mean Square) value ranging from 0.2 s.d 0.5. There are three subduction of the part in south sumatra. The subduction zone formed in Bengkulu is about 26.78º, the subduction zone of Lampung is around 30.225º and the subduction of the Sunda Strait is about 52.53º. Subduction zone of Bengkulu at depth of 250 km, Lampung and Sunda Strait at depth 400 km.
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JGE
JGE
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