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Jurnal

MIKROZONASI KAWASAN RAWAN BENCANA GEMPABUMI DENGAN STUDI PEAK GROUND ACCELERATION MENGGUNAKAN METODE BOORE ATKINSON DAN DATA MIKROTREMOR DI DAERAH KUPANG

JURNAL GEOCELEBES · Vol. 1 No. 1 (2017) · pp. 5–12

DOI
10.20956/geocelebes.v1i1.1774
ISSN
2579-5546, 2579-5821
Published
2017-05-02
Publisher
Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar
Language
en

Abstract

AbstrakLetak geografis Indonesia yang berada pada pertemuan tiga lempeng tektonik utama; Lempeng Indo-Australia, Lempeng Eurasia dan Lempeng Pasifik, menjadikan Indonesia sebagai kawasan rawan gempabumi. Berdasarkan data yang dirilis oleh Direktorat Vulkanologi dan Mitigasi Bencana Geologi (DVMBG) terdapat 28 wilayah rawan gempa dan tsunami termasuk Kupang. Kupang terletak di zona busur sangat aktif dan tepian benua aktif. Kegiatan tektonik yang berlangsung saat ini dicirikan dengan kejadian gempa tektonik yang melanda daerah pedalaman, akibat dari aktifnya sesar-sesar yang terdapat di perbukitan sekitar Kota Kupang. Salah satu upaya mitigasi yang dilakukan adalah pengukuran mikrotremor menggunakan metode HVSR (Horizontal to Vertical Spectral Ratio) untuk mengetahui nilai frekuensi dominan yang akan menjadi penentu tingkat kerawanan bencana gempabumi. Nilai frekuensi dominan akan menghitung nilai kecepatan gelombang S hingga kedalaman 30 meter (Vs30) yang selanjtnya digunakan untuk menentukan nilai PGA dan amplifikasi. Hasil analisis data menunjukkan bahwa nilai periode dominan berada pada rentang 0.1-0.97 sekon, nilai PGA antara 92.87-142.84 gal dan nilai amplifikasi adalah 0.99-4.38 dan 2.12-9.43 kali. Maka dapat disimpulkan bahwa daerah penelitian termasuk kategori rawan bencana gempabumi terutama pada bagian tenggara.Kata Kunci: Amplifikasi, Mikrotremor, Periode Dominan, PGAAbstractGeographically, Indonesia located at the meeting of three major tectonic plates; Indo-Australian Plate, Eurasian Plate, and Pacific Plate, that make Indonesia as earthquake-prone area. Based on data released by the Directorate of Volcanology and Geological Hazard Mitigation (DVMBG), there are 28 earthquake and tsunami prone areas including Kupang that the area located in the very active arc zone and the edge of the active continent. The tectonic activity that is currently taking place is characterized by the tectonic earthquake that attacks to countryside areas, resulting from the active fault-faults found in the hills around the area. One of the mitigation efforts is microtremor measurement using HVSR (Horizontal to Vertical Spectral Ratio) method to find out the dominant frequency for determination of the magnitude of the earthquake. The predominant frequency value will determine the Shear wave velocity up to 30 meters (Vs30) which are further used for the PGA and amplification values. The result of data analysis shows that the dominant period value is in the range 0.1-0.97 second, PGA value between 92.87-142.84 gal and the amplification value is 0.99-4.38 and 2.12-9.43 times. The conclusion, the area is categorized as earthquake-prone, especially in the southeast region.Keywords: Amplification, Microtremor, Dominant Period, PGA

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Co-authorOrganisationJoint articles
Muh. Altin MassinaiAffiliation unknown2
Fitriani FitrianiAffiliation unknown2
Marjiyono MarjiyonoAffiliation unknown2
Johannes Gedo SeaAffiliation unknown1
Yusuf Surachman DjajadihardjaAffiliation unknown1
Nur Hidayat NurdinAffiliation unknown1
Syamsuddin SyamsuddinAffiliation unknown1
A. Hardianti YunusAffiliation unknown1
Muhammad ZulfitrahAffiliation unknown1
Syamsuddin SyamsuddinAffiliation unknown1
Jamaluddin JamaluddinAffiliation unknown1
Wahyuni WahyuniAffiliation unknown1
La Ode ArminAffiliation unknown1
Bambang harimei SupraptoAffiliation unknown1
Samsu ArifAffiliation unknown1
Iswar Edis PratamaAffiliation unknown1
Indra Jaya MuhtarAffiliation unknown1
Syamsuddin SyamsuddinAffiliation unknown1
Syamsuddin SyamsuddinAffiliation unknown1
Titien HaryaniAffiliation unknown1
Riyadi RiyadiAffiliation unknown1
Marniati RamliAffiliation unknown1

Affiliations come from OpenAlex; journal OAI-PMH metadata carries none. Authors without an OpenAlex ID are matched by name, which can merge or split people.

Metadata source: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/geocelebes/oai, first harvested 3 Nov 2026, last seen 3 Nov 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en">MIKROZONASI KAWASAN RAWAN BENCANA GEMPABUMI DENGAN STUDI PEAK GROUND ACCELERATION MENGGUNAKAN METODE BOORE ATKINSON DAN DATA MIKROTREMOR DI DAERAH KUPANG</dc:title>
	<dc:creator xml:lang="en">Jamal, Rachmat Jariah</dc:creator>
	<dc:creator xml:lang="en">Lantu, Lantu</dc:creator>
	<dc:creator xml:lang="en">Aswad, Sabrianto</dc:creator>
	<dc:creator xml:lang="en">Sulaiman, Cecep</dc:creator>
	<dc:description xml:lang="en">AbstrakLetak geografis Indonesia yang berada pada pertemuan tiga lempeng tektonik utama; Lempeng Indo-Australia, Lempeng Eurasia dan Lempeng Pasifik, menjadikan Indonesia sebagai kawasan rawan gempabumi. Berdasarkan data yang dirilis oleh Direktorat Vulkanologi dan Mitigasi Bencana Geologi (DVMBG) terdapat 28 wilayah rawan gempa dan tsunami termasuk Kupang. Kupang terletak di zona busur sangat aktif dan tepian benua aktif. Kegiatan tektonik yang berlangsung saat ini dicirikan dengan kejadian gempa tektonik yang melanda daerah pedalaman, akibat dari aktifnya sesar-sesar yang terdapat di perbukitan sekitar Kota Kupang. Salah satu upaya mitigasi yang dilakukan adalah pengukuran mikrotremor menggunakan metode HVSR (Horizontal to Vertical Spectral Ratio) untuk mengetahui nilai frekuensi dominan yang akan menjadi penentu tingkat kerawanan bencana gempabumi. Nilai frekuensi dominan akan menghitung nilai kecepatan gelombang S hingga kedalaman 30 meter (Vs30) yang selanjtnya digunakan untuk menentukan nilai PGA dan amplifikasi. Hasil analisis data menunjukkan bahwa nilai periode dominan berada pada rentang 0.1-0.97 sekon, nilai PGA antara 92.87-142.84 gal dan nilai amplifikasi adalah 0.99-4.38 dan 2.12-9.43 kali. Maka dapat disimpulkan bahwa daerah penelitian termasuk kategori rawan bencana gempabumi terutama pada bagian tenggara.Kata Kunci : Amplifikasi, Mikrotremor, Periode Dominan, PGAAbstractGeographically, Indonesia located at the meeting of three major tectonic plates; Indo-Australian Plate, Eurasian Plate, and Pacific Plate, that make Indonesia as earthquake-prone area. Based on data released by the Directorate of Volcanology and Geological Hazard Mitigation (DVMBG), there are 28 earthquake and tsunami prone areas including Kupang that the area located in the very active arc zone and the edge of the active continent. The tectonic activity that is currently taking place is characterized by the tectonic earthquake that attacks to countryside areas, resulting from the active fault-faults found in the hills around the area. One of the mitigation efforts is microtremor measurement using HVSR (Horizontal to Vertical Spectral Ratio) method to find out the dominant frequency for determination of the magnitude of the earthquake. The predominant frequency value will determine the Shear wave velocity up to 30 meters (Vs30) which are further used for the PGA and amplification values. The result of data analysis shows that the dominant period value is in the range 0.1-0.97 second, PGA value between 92.87-142.84 gal and the amplification value is 0.99-4.38 and 2.12-9.43 times. The conclusion, the area is categorized as earthquake-prone, especially in the southeast region.Keywords: Amplification, Microtremor, Dominant Period, PGA</dc:description>
	<dc:publisher xml:lang="en">Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar</dc:publisher>
	<dc:date>2017-05-02</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.unhas.ac.id/index.php/geocelebes/article/view/1774</dc:identifier>
	<dc:identifier>10.20956/geocelebes.v1i1.1774</dc:identifier>
	<dc:source xml:lang="en">JURNAL GEOCELEBES; Vol. 1 No. 1: April 2017; 5-12</dc:source>
	<dc:source>2579-5546</dc:source>
	<dc:source>2579-5821</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/geocelebes/article/view/1774/1014</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2017 JURNAL GEOCELEBES</dc:rights>
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