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Interpretasi Tingkat Kekerasan Batuan Bawah Permukaan di Daerah Rawan Gempa Bumi Kota Bengkulu

INDONESIAN JOURNAL OF APPLIED PHYSICS · Vol. 11 No. 1 (2021) · hlm. 11–24

DOI
10.13057/ijap.v11i1.46525
ISSN
2477-6416, 2089-0133
Terbit
2021-04-30
Penerbit
Department of Physics, Sebelas Maret University
Bahasa
eng

Abstrak

Bengkulu City is located in the subduction zone of the Indo-Australian and Eurasian plates, so it is prone to earthquake. To anticipate the impact of earthquake, disaster mitigation can be carried out, one of which is a study of the level of rock hardness in the area. This study aims to determine the level of rock hardness based on seismic wave velocity in several rock formations and to determine which rock formations have the potential to cause vulnerability to earthquakes. Field data acquisition uses the seismic refraction method with time-term inversion technique. The data obtained in the field are processed to obtain a 2-D cross-section of the subsurface seismic wave velocity values. The study results show that the level of rock hardness depends on the type of rock formation. The Andesite Rock Formation Unit (Tpan) has the highest level of hardness, while the transitional area between the Alluvium Rock Formation Unit (Qa) and the Swamp Sedimentary Rock Formation Unit (Qs) has the lowest level of hardness.

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  • University of Bengkulu
  • Meteorological, Climatological, And Geophysical Agency
  • Universitas Syiah Kuala
  • Afiliasi tidak diketahui
  • Organisasi berbeda
  • Organisasi sama
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Rekan penulisOrganisasiArtikel bersama
Hana RaihanaUniversity of Bengkulu7
Andre Rahmat Al AnsoryUniversity of Bengkulu5
Suhendra SuhendraUniversity of Bengkulu4
Muchammad FaridUniversity of Bengkulu4
Darmawan Ikhlas FadliUniversity of Bengkulu2
Jesika Erni Elfrita SinagaUniversity of Bengkulu2
Rida SamdaraUniversity of Bengkulu2
RefrizonUniversity of Bengkulu2
Khairun NazliUniversitas Syiah Kuala2
Aisyah Cindy Phylia PutriUniversity of Bengkulu2
Nanang SugiantoUniversity of Bengkulu2
Nurul ApriyantiUniversity of Bengkulu2
Ulfa NuramadaniUniversity of Bengkulu1
Ardika Pratama PanjaitanUniversity of Bengkulu1
Muhammad FaridUniversity of Bengkulu1
Nurul Ilmi RahmawatiUniversity of Bengkulu1
Ainul LisaUniversity of Bengkulu1
Siti Hanifah MaulaniUniversity of Bengkulu1
Lori Agung SatriaMeteorological, Climatological, And Geophysical Agency1
Suaidi AhadiMeteorological, Climatological, And Geophysical Agency1
Muhammad Rifqi RabbaniUniversity of Bengkulu1
Budi HarliantoUniversity of Bengkulu1
Arya Putra AnggiUniversity of Bengkulu1
Bayu Saputra Bayu SaputraAfiliasi tidak diketahui1
Bimantara Panca Utama Bimantara Panca UtamaAfiliasi tidak diketahui1
Wahyu Cahyadi Setiawan SetiawanUniversity of Bengkulu1
Suhendra SuhendraUniversity of Bengkulu1
Muhammad Wilzam Fauzi Muhammad Wilzam FauziUniversity of Bengkulu1
Sri Rahayu Sri RahayuUniversity of Bengkulu1
Rival Zamrawi Rival ZamrawiUniversity of Bengkulu1
Dadin Mars AbimayuUniversity of Bengkulu1
Sapari DwiyonoAfiliasi tidak diketahui1
Arieffin Yusuf Hakim HakimUniversity of Bengkulu1
Asy Syifa Auliya Putri RamadhaniUniversity of Bengkulu1
Samuel SiagianUniversity of Bengkulu1

Afiliasi berasal dari OpenAlex; metadata OAI-PMH jurnal tidak memuatnya. Penulis tanpa ID OpenAlex dicocokkan berdasarkan nama, sehingga dua orang bisa tergabung atau satu orang bisa terpisah.

Sumber metadata: OAI-PMH (metadata jurnal) https://jurnal.uns.ac.id/ijap/oai, pertama di-harvest 8 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc)
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	<dc:title xml:lang="en-US">Interpretasi Tingkat Kekerasan Batuan Bawah Permukaan di Daerah Rawan Gempa Bumi Kota Bengkulu</dc:title>
	<dc:creator>Hadi, Arif Ismul</dc:creator>
	<dc:creator>Refrizon, Refrizon</dc:creator>
	<dc:creator>Halauddin, Halauddin</dc:creator>
	<dc:creator>Lidiawati, Liza</dc:creator>
	<dc:creator>Edo, Paisal</dc:creator>
	<dc:subject xml:lang="en-US">Bengkulu City; earthquake; rock hardness; time-term inversion; vulnerability</dc:subject>
	<dc:description xml:lang="en-US">Bengkulu City is located in the subduction zone of the Indo-Australian and Eurasian plates, so it is prone to earthquake. To anticipate the impact of earthquake, disaster mitigation can be carried out, one of which is a study of the level of rock hardness in the area. This study aims to determine the level of rock hardness based on seismic wave velocity in several rock formations and to determine which rock formations have the potential to cause vulnerability to earthquakes. Field data acquisition uses the seismic refraction method with time-term inversion technique. The data obtained in the field are processed to obtain a 2-D cross-section of the subsurface seismic wave velocity values. The study results show that the level of rock hardness depends on the type of rock formation. The Andesite Rock Formation Unit (Tpan) has the highest level of hardness, while the transitional area between the Alluvium Rock Formation Unit (Qa) and the Swamp Sedimentary Rock Formation Unit (Qs) has the lowest level of hardness.</dc:description>
	<dc:publisher xml:lang="en-US">Department of Physics, Sebelas Maret University</dc:publisher>
	<dc:contributor xml:lang="en-US">Geophysics Study Program, Physics Department, Faculty of Mathematics and Natural Sciences, University of Bengkulu</dc:contributor>
	<dc:date>2021-04-30</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-US">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://jurnal.uns.ac.id/ijap/article/view/46525</dc:identifier>
	<dc:identifier>10.13057/ijap.v11i1.46525</dc:identifier>
	<dc:source xml:lang="en-US">INDONESIAN JOURNAL OF APPLIED PHYSICS; Vol 11, No 1 (2021): April; 11-24</dc:source>
	<dc:source>2477-6416</dc:source>
	<dc:source>2089-0133</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://jurnal.uns.ac.id/ijap/article/view/46525/31429</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2021 INDONESIAN JOURNAL OF APPLIED PHYSICS</dc:rights>
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