PENENTUAN PATAHAN DAN TOPOGRAFI MOHO PADA DATA NOAA-FA BERBASIS FFT
| Main Author: | Bagus Jaya Santosa, Sungkono, |
|---|---|
| Format: | Article info application/pdf eJournal |
| Bahasa: | eng |
| Terbitan: |
Department of Physics, Maulana Malik Ibrahim State Islamic University of Malang
, 2012
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| Subjects: | |
| Online Access: |
http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638 http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638/2907 http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638/2908 |
| ctrlnum |
article-1638 |
|---|---|
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<dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><title lang="en-US">PENENTUAN PATAHAN DAN TOPOGRAFI MOHO PADA DATA NOAA-FA BERBASIS FFT</title><creator>Bagus Jaya Santosa, Sungkono,</creator><subject lang="en-US">Saintek; fisika</subject><subject lang="en-US">Gravity; FFT; Inversion; Fault; Fracture; Moho</subject><description lang="en-US">Regional Gravity NOAA-FA data analysis using several gradient methods has been conducted to determine the fracture and direction fault based on FFT. Fault can be qualitatively identified from a regional anomaly data, gradient Theta and  Normalized Standard Deviation (NSD)  is  trending  north-south.  Dominant  fracture  orientation  parallel  to  the  fault  is  only detectable by gradient Theta and NSD, but  more  obviously displayed on the gradient NSD. Furthermore, regional anomaly of  Gravity data  inverted to generate  Moho  topography. This inversion  using  FFT  based  algorithm  (Parker,  1972).  The  inversion  result  of  Moho  depths between 30-39  km.  In the Moho  topography, there is contrast  depth  difference, namely the Latitude -35 to -25 and Longitude -70 to -65, which is suspected as a fracture.Keyword: Gravity, FFT, Inversion, Fault, Fracture, Moho</description><publisher lang="en-US">Department of Physics, Maulana Malik Ibrahim State Islamic University of Malang</publisher><contributor lang="en-US"/><date>2012-03-28</date><type>Journal:Article</type><type>Other:info:eu-repo/semantics/publishedVersion</type><type>Journal:Article</type><type>File:application/pdf</type><type>File:application/pdf</type><identifier>http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638</identifier><identifier>10.18860/neu.v0i0.1638</identifier><source lang="en-US">Jurnal Neutrino:Jurnal Fisika dan Aplikasinya; JURNAL NEUTRINO (Vol 2 No 2; 04-2010)</source><source>2460-5999</source><source>1979-6374</source><language>eng</language><relation>http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638/2907</relation><relation>http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638/2908</relation><recordID>article-1638</recordID></dc>
|
| language |
eng |
| format |
Journal:Article Journal Other:info:eu-repo/semantics/publishedVersion Other File:application/pdf File Journal:eJournal |
| author |
Bagus Jaya Santosa, Sungkono, |
| title |
PENENTUAN PATAHAN DAN TOPOGRAFI MOHO PADA DATA NOAA-FA BERBASIS FFT |
| publisher |
Department of Physics, Maulana Malik Ibrahim State Islamic University of Malang |
| publishDate |
2012 |
| topic |
Saintek fisika Gravity FFT Inversion Fault Fracture Moho |
| url |
http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638 http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638/2907 http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/1638/2908 |
| contents |
Regional Gravity NOAA-FA data analysis using several gradient methods has been conducted to determine the fracture and direction fault based on FFT. Fault can be qualitatively identified from a regional anomaly data, gradient Theta and Normalized Standard Deviation (NSD) is trending north-south. Dominant fracture orientation parallel to the fault is only detectable by gradient Theta and NSD, but more obviously displayed on the gradient NSD. Furthermore, regional anomaly of Gravity data inverted to generate Moho topography. This inversion using FFT based algorithm (Parker, 1972). The inversion result of Moho depths between 30-39 km. In the Moho topography, there is contrast depth difference, namely the Latitude -35 to -25 and Longitude -70 to -65, which is suspected as a fracture.Keyword: Gravity, FFT, Inversion, Fault, Fracture, Moho |
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IOS2733.article-1638 |
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Universitas Islam Negeri Maulana Malik Ibrahim Malang |
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mill.onesearch.id fkp2tn.onesearch.id ptki.onesearch.id |
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Perpustakaan UIN Maulana Malik Ibrahim Malang |
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504 |
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Jurnal Neutrino : Jurnal Fisika Dan Aplikasinya |
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2733 |
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Fisika |
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MALANG |
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JAWA TIMUR |
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2017-02-25T15:10:40Z |
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