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Analisa Receiver Function Teleseismic untuk Mendeteksi Moho pada Stasiun Bkb Data Meramex

INDONESIAN JOURNAL OF APPLIED PHYSICS · Vol. 3 No. 02 (2016) · pp. 195–200

DOI
10.13057/ijap.v3i02.1272
ISSN
2477-6416, 2089-0133
Published
2016-05-21
Publisher
Department of Physics, Sebelas Maret University
Language
eng

Abstract

It has been done a research to determine internal earth using receiver function teleseismic analysis method. This method have been done by using MERAMEX (MErapi Amphibious Experiment) data from broadband seismometer BKB. Event of teleseismic is chosen from Honshu Japan with radius 30o and magnitude 7.2. This research begun by analysing radial and vertical characteristic of teleseismic eventand using bandpass filter with range 0.003 Hz – 0.5 Hz. Then Iteractive Deconvolution is used to get velocity model. The result of this model shows crustal model that has 4 Km thick upper crust, a 26 Km thick lower crust and 10 Km thick Moho transition zone, with velocity increasing gradually.

Collaboration network of the authors

32 authors · 146 co-authorship links · 13 across different organisations

Hover or tap a name to highlight its co-authors. Double-click to open the author's page.

  • STMIK Bina Patria
  • Bandung Institute of Technology
  • IPB University
  • King Abdulaziz University
  • Universitas Trisakti
  • Affiliation unknown
  • Different organisations
  • Same organisation
  • Affiliation unknown
  • Thicker line = more joint articles · bigger circle = more articles
Show as table
Co-authorOrganisationJoint articles
Sugeng Sapto SurjonoAffiliation unknown2
Donatus Hendra AmijayaAffiliation unknown2
Yeza FebrianiSTMIK Bina Patria1
Mohammad ApriniyadiUniversitas Trisakti1
Muhammad Lutfi Mahasinul AkhlakSTMIK Bina Patria1
Satriya Yudha WiratamaSTMIK Bina Patria1
Wahyu SrigutomoBandung Institute of Technology1
Nina Siti AminahBandung Institute of Technology1
Mitra DjamalBandung Institute of Technology1
Irwan MeilanoAffiliation unknown1
Ari SetiawanAffiliation unknown1
Irzaman IrzamanIPB University1
Perdinan PerdinanIPB University1
Retna ApsariAffiliation unknown1
Imam SuyantoAffiliation unknown1
Heriansyah PutraAffiliation unknown1
Herlan DarmawanAffiliation unknown1
Maria EvitaAffiliation unknown1
Moh YasinAffiliation unknown1
Wahyudi WahyudiAffiliation unknown1
Leni Sophia HelianiAffiliation unknown1
Hidayat PanuntunAffiliation unknown1
Cecep PratamaAffiliation unknown1
Saptono Budi SamodraAffiliation unknown1
Budi PurnamaAffiliation unknown1
Budi LegowoAffiliation unknown1
Artono Dwijo SutomoAffiliation unknown1
Anti Fatkhul QoiriahAffiliation unknown1
Shandiyano PutraAffiliation unknown1
Sarju WinardiAffiliation 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://jurnal.uns.ac.id/ijap/oai, first harvested 8 Nov 2026, last seen 8 Nov 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en-US">Analisa Receiver Function Teleseismic untuk Mendeteksi Moho pada Stasiun Bkb Data Meramex</dc:title>
	<dc:creator>Amukti, Rian</dc:creator>
	<dc:creator>Suryanto, Wiwit</dc:creator>
	<dc:description xml:lang="en-US">It has been done a research to determine internal earth using receiver function teleseismic analysis method. This method have been done by using MERAMEX (MErapi Amphibious Experiment) data from broadband seismometer BKB. Event of teleseismic is chosen from Honshu Japan with radius 30o and magnitude 7.2. This research begun by analysing radial and vertical characteristic of teleseismic eventand using bandpass filter with range 0.003 Hz – 0.5 Hz. Then Iteractive Deconvolution is used to get velocity model. The result of this model shows crustal model that has 4 Km thick upper crust, a 26 Km thick lower crust and 10 Km thick Moho transition zone, with velocity increasing gradually.</dc:description>
	<dc:publisher xml:lang="en-US">Department of Physics, Sebelas Maret University</dc:publisher>
	<dc:contributor xml:lang="en-US"></dc:contributor>
	<dc:date>2016-05-21</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/1272</dc:identifier>
	<dc:identifier>10.13057/ijap.v3i02.1272</dc:identifier>
	<dc:source xml:lang="en-US">INDONESIAN JOURNAL OF APPLIED PHYSICS; Vol 3, No 02 (2013): October; 195-200</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/1272/1214</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2016 INDONESIAN JOURNAL OF APPLIED PHYSICS</dc:rights>
</oai_dc:dc>