IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIK

Gravity method generally can read the difference of rock density to identify subsurface structures. This research was conducted in Riau area with the aim of knowing fault and subsurface structure, and determining sub-basin boundary. Data processing was done by using spectral analysis, SHD and SVD an...

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Main Authors: Wuri Andari, Karyanto Karyanto, Riski Kurniawan
Format: Article
Language:English
Published: Jurusan Teknik Geofisika Fakultas Teknik Universitas Lampung 2020-01-01
Series:JGE
Subjects:
svd
shd
Online Access:https://jge.eng.unila.ac.id/index.php/geoph/article/view/23
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spelling doaj-324f4315b4144e5e988dcfb1afa383052021-07-08T09:35:19ZengJurusan Teknik Geofisika Fakultas Teknik Universitas LampungJGE2356-15992685-61822020-01-0151607410.23960/jge.v5i1.2328IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIKWuri Andari0Karyanto Karyanto1Riski Kurniawan2Universitas LampungUniversitas LampungChevron Pasivic IndonesiaGravity method generally can read the difference of rock density to identify subsurface structures. This research was conducted in Riau area with the aim of knowing fault and subsurface structure, and determining sub-basin boundary. Data processing was done by using spectral analysis, SHD and SVD analysis, and 2D modeling then later correlated with seismic section to find out the subsurface structure of research area. The results showed that the bouguer anomaly value had a range of values between 5.6 mGal to 33.2 mGal with a surface density of 1.95 g / cc. High anomaly were in the eastern region and low anomaly were in the NW - SE trending region. 6 low anomalies indicated as a sub-basin pattern were separated by a relatively high altitude area of North West Southeast. The average residual anomaly depth was about 2.3 km. Based on the 2D subsurface modeling results, there was layer structure from the youngest to eldest that were alluvial deposits, Petani Formation, Sihapas group and granitic rock as the base rock. The projected subsurface section to surface showed 5 sub-basins with basin width 4-12 km located in the sub-basin and fault indication area.https://jge.eng.unila.ac.id/index.php/geoph/article/view/23sub-basinsvdshdgravityseismic
collection DOAJ
language English
format Article
sources DOAJ
author Wuri Andari
Karyanto Karyanto
Riski Kurniawan
spellingShingle Wuri Andari
Karyanto Karyanto
Riski Kurniawan
IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIK
JGE
sub-basin
svd
shd
gravity
seismic
author_facet Wuri Andari
Karyanto Karyanto
Riski Kurniawan
author_sort Wuri Andari
title IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIK
title_short IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIK
title_full IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIK
title_fullStr IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIK
title_full_unstemmed IDENTIFIKASI BATAS SUB-CEKUNGAN HIDROKARBON MENGGUNAKAN ANALISIS SHD (SECOND HORIZONTAL DERIVATIVE) DAN SVD (SECOND VERTICAL DERIVATIVE) BERDASARKAN KORELASI DATA GAYABERAT DAN SEISMIK
title_sort identifikasi batas sub-cekungan hidrokarbon menggunakan analisis shd (second horizontal derivative) dan svd (second vertical derivative) berdasarkan korelasi data gayaberat dan seismik
publisher Jurusan Teknik Geofisika Fakultas Teknik Universitas Lampung
series JGE
issn 2356-1599
2685-6182
publishDate 2020-01-01
description Gravity method generally can read the difference of rock density to identify subsurface structures. This research was conducted in Riau area with the aim of knowing fault and subsurface structure, and determining sub-basin boundary. Data processing was done by using spectral analysis, SHD and SVD analysis, and 2D modeling then later correlated with seismic section to find out the subsurface structure of research area. The results showed that the bouguer anomaly value had a range of values between 5.6 mGal to 33.2 mGal with a surface density of 1.95 g / cc. High anomaly were in the eastern region and low anomaly were in the NW - SE trending region. 6 low anomalies indicated as a sub-basin pattern were separated by a relatively high altitude area of North West Southeast. The average residual anomaly depth was about 2.3 km. Based on the 2D subsurface modeling results, there was layer structure from the youngest to eldest that were alluvial deposits, Petani Formation, Sihapas group and granitic rock as the base rock. The projected subsurface section to surface showed 5 sub-basins with basin width 4-12 km located in the sub-basin and fault indication area.
topic sub-basin
svd
shd
gravity
seismic
url https://jge.eng.unila.ac.id/index.php/geoph/article/view/23
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AT karyantokaryanto identifikasibatassubcekunganhidrokarbonmenggunakananalisisshdsecondhorizontalderivativedansvdsecondverticalderivativeberdasarkankorelasidatagayaberatdanseismik
AT riskikurniawan identifikasibatassubcekunganhidrokarbonmenggunakananalisisshdsecondhorizontalderivativedansvdsecondverticalderivativeberdasarkankorelasidatagayaberatdanseismik
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