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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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 |
work_keys_str_mv |
AT wuriandari identifikasibatassubcekunganhidrokarbonmenggunakananalisisshdsecondhorizontalderivativedansvdsecondverticalderivativeberdasarkankorelasidatagayaberatdanseismik AT karyantokaryanto identifikasibatassubcekunganhidrokarbonmenggunakananalisisshdsecondhorizontalderivativedansvdsecondverticalderivativeberdasarkankorelasidatagayaberatdanseismik AT riskikurniawan identifikasibatassubcekunganhidrokarbonmenggunakananalisisshdsecondhorizontalderivativedansvdsecondverticalderivativeberdasarkankorelasidatagayaberatdanseismik |
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1721313521473421312 |