Microtremors Measurement Around Dengkeng Fault Line in Central Java

D. Darmawan, M. I. N. Hafsyah, N. B. Wibowo, L. Katriani, K. N. Aziz, Siti Patimah, Rofiki, B. Ruwanto
{"title":"Microtremors Measurement Around Dengkeng Fault Line in Central Java","authors":"D. Darmawan, M. I. N. Hafsyah, N. B. Wibowo, L. Katriani, K. N. Aziz, Siti Patimah, Rofiki, B. Ruwanto","doi":"10.2991/ASSEHR.K.210305.059","DOIUrl":null,"url":null,"abstract":"Microtremor signals measurement had been conducted in area surrounding Dengkeng Fault line in Central Java, Indonesia. This research is aimed to identify the characteristics of area surrounding Dengkeng fault line and to identify the Dengkeng fault line through microtremors parameters analysis. Microtremor signals were obtained from field measurement using TDV-23/TDL-303 Taide Digital Portable Seismograph and were analyzed using Horizontal to Vertical Spectral Ratio (HVSR) method. There were 48 stations with 2 km spacing between stations that covers the area around Dengkeng fault line. The results showed that the microzonation of microtremor parameters in the area around Dengkeng Fault line are in good agreement with the geological setting of the research area depicted in official geological map. They also showed that Dengkeng Fault line is located in geological formation boundary between Gunungapi Merapi Muda formation and Kebobutak formation as previously predicted and mostly striking East-West.","PeriodicalId":378773,"journal":{"name":"Proceedings of the 7th International Conference on Research, Implementation, and Education of Mathematics and Sciences (ICRIEMS 2020)","volume":"181 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of the 7th International Conference on Research, Implementation, and Education of Mathematics and Sciences (ICRIEMS 2020)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2991/ASSEHR.K.210305.059","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Microtremor signals measurement had been conducted in area surrounding Dengkeng Fault line in Central Java, Indonesia. This research is aimed to identify the characteristics of area surrounding Dengkeng fault line and to identify the Dengkeng fault line through microtremors parameters analysis. Microtremor signals were obtained from field measurement using TDV-23/TDL-303 Taide Digital Portable Seismograph and were analyzed using Horizontal to Vertical Spectral Ratio (HVSR) method. There were 48 stations with 2 km spacing between stations that covers the area around Dengkeng fault line. The results showed that the microzonation of microtremor parameters in the area around Dengkeng Fault line are in good agreement with the geological setting of the research area depicted in official geological map. They also showed that Dengkeng Fault line is located in geological formation boundary between Gunungapi Merapi Muda formation and Kebobutak formation as previously predicted and mostly striking East-West.
中爪哇登坑断裂带周边微震测量
在印度尼西亚中爪哇登坑断裂带周边地区进行了微震信号测量。本研究旨在通过微震参数分析,识别登坑断裂带周边区域特征,识别登坑断裂带。利用TDV-23/TDL-303台德数字便携式地震仪现场测量得到微震信号,并用水平与垂直频谱比(HVSR)方法进行分析。在登坑断裂带附近,共设48个测点,测点间距为2公里。结果表明,登坑断裂带周边地区微震参数的微带性与官方地质图所描绘的研究区地质背景吻合较好。结果表明,登坑断裂线位于Gunungapi Merapi Muda组与Kebobutak组的地质构造界线上,与前人预测一致,且以东西走向为主。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信