Microseismic Signals In The Obs Meramex Data Recording

In order to detennine the frequency content especially microseismic in the data recording of ocean bottom seismo­ graph Meramex; an analysis has been conducted by comparing the OBS data recording when earthquakes occured with local and regional distants (6") on 27 and 28 June 2004, an...

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Main Authors: Gatot, Yuliyanto, Kirbani, Sri Brotopuspito, Wiwit, Suryanto
Format: Article
Language:English
Published: Physics Department Sebelas Maret University 2011
Subjects:
Online Access:https://repository.ugm.ac.id/97166/1/13.pdf
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author Gatot, Yuliyanto
Kirbani, Sri Brotopuspito
Wiwit, Suryanto
author_facet Gatot, Yuliyanto
Kirbani, Sri Brotopuspito
Wiwit, Suryanto
author_sort Gatot, Yuliyanto
collection UGM
description In order to detennine the frequency content especially microseismic in the data recording of ocean bottom seismo­ graph Meramex; an analysis has been conducted by comparing the OBS data recording when earthquakes occured with local and regional distants (6") on 27 and 28 June 2004, and also the comparison with the seismograph signal on the land. The analysis is conducted by processing the amplitude spectra from the data recording using geopsy software. The result obtained from the analysis is that the characteristic frequency content in the OBS is dominated by the maximum amplitude-: t-fr.:q ;ency 0.15 Hz for both data with and without earthquake event, whereas from the earthquake data recording station on the land (Al3 and AJI) drew a result on the peak amplitudo at the frequency about 0.3 Hz. or in the other words, the seismic recording data both in the station and OBS have the peak frequency which is near the microseismic peak frequency.
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spelling oai:generic.eprints.org:971662015-02-16T04:11:58Z https://repository.ugm.ac.id/97166/ Microseismic Signals In The Obs Meramex Data Recording Gatot, Yuliyanto Kirbani, Sri Brotopuspito Wiwit, Suryanto Classical Physics In order to detennine the frequency content especially microseismic in the data recording of ocean bottom seismo­ graph Meramex; an analysis has been conducted by comparing the OBS data recording when earthquakes occured with local and regional distants (6") on 27 and 28 June 2004, and also the comparison with the seismograph signal on the land. The analysis is conducted by processing the amplitude spectra from the data recording using geopsy software. The result obtained from the analysis is that the characteristic frequency content in the OBS is dominated by the maximum amplitude-: t-fr.:q ;ency 0.15 Hz for both data with and without earthquake event, whereas from the earthquake data recording station on the land (Al3 and AJI) drew a result on the peak amplitudo at the frequency about 0.3 Hz. or in the other words, the seismic recording data both in the station and OBS have the peak frequency which is near the microseismic peak frequency. Physics Department Sebelas Maret University 2011-03-08 Article PeerReviewed application/pdf en https://repository.ugm.ac.id/97166/1/13.pdf Gatot, Yuliyanto and Kirbani, Sri Brotopuspito and Wiwit, Suryanto (2011) Microseismic Signals In The Obs Meramex Data Recording. Proceedings Kentingan Physics Forum Acoustics Geophysics Cluster Meeting 2011. pp. 33-37. ISSN 979-978-3456-83-8 (In Press)
spellingShingle Classical Physics
Gatot, Yuliyanto
Kirbani, Sri Brotopuspito
Wiwit, Suryanto
Microseismic Signals In The Obs Meramex Data Recording
title Microseismic Signals In The Obs Meramex Data Recording
title_full Microseismic Signals In The Obs Meramex Data Recording
title_fullStr Microseismic Signals In The Obs Meramex Data Recording
title_full_unstemmed Microseismic Signals In The Obs Meramex Data Recording
title_short Microseismic Signals In The Obs Meramex Data Recording
title_sort microseismic signals in the obs meramex data recording
topic Classical Physics
url https://repository.ugm.ac.id/97166/1/13.pdf
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AT kirbanisribrotopuspito microseismicsignalsintheobsmeramexdatarecording
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