INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI

Research using the gravity method applied in Way Umpu geothermal area to identify geothermal system. Regional anomalies and the residual anomalies were separated using upward continuation method with an altitude of 1000 meters. Subsurface structure modelling was made by the residual anomalies. Then...

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Main Authors: , MUKHAMAD FARDIAN HATARI SATRIA, , Drs. Imam Suyanto, M.Si.
Format: Thesis
Published: [Yogyakarta] : Universitas Gadjah Mada 2014
Subjects:
ETD
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author , MUKHAMAD FARDIAN HATARI SATRIA
, Drs. Imam Suyanto, M.Si.
author_facet , MUKHAMAD FARDIAN HATARI SATRIA
, Drs. Imam Suyanto, M.Si.
author_sort , MUKHAMAD FARDIAN HATARI SATRIA
collection UGM
description Research using the gravity method applied in Way Umpu geothermal area to identify geothermal system. Regional anomalies and the residual anomalies were separated using upward continuation method with an altitude of 1000 meters. Subsurface structure modelling was made by the residual anomalies. Then they were correlated with the geological data and the fault analysis result using the second vertical derivative (SVD). The model shows that the lithology consist of basaltic lava with density 2,9 gr/cc. It was the result of the Pungur vulcano activities. Basaltic breccia with density 2,65 gr/cc is interpreted as a geothermal reservoir, andesite lava with density 2,8 gr/cc is analyzed as the result of the activity of Mt. Remas which plays as the cap rock and andesite breccia with density 2,6 gr/cc.That lithology are being covered by alluvial rock with density 1,9 gr/cc Keyword : gravity method, SVD, modelling, geothermal
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institution Universiti Gadjah Mada
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spelling oai:generic.eprints.org:1310602016-03-04T08:01:29Z https://repository.ugm.ac.id/131060/ INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI , MUKHAMAD FARDIAN HATARI SATRIA , Drs. Imam Suyanto, M.Si. ETD Research using the gravity method applied in Way Umpu geothermal area to identify geothermal system. Regional anomalies and the residual anomalies were separated using upward continuation method with an altitude of 1000 meters. Subsurface structure modelling was made by the residual anomalies. Then they were correlated with the geological data and the fault analysis result using the second vertical derivative (SVD). The model shows that the lithology consist of basaltic lava with density 2,9 gr/cc. It was the result of the Pungur vulcano activities. Basaltic breccia with density 2,65 gr/cc is interpreted as a geothermal reservoir, andesite lava with density 2,8 gr/cc is analyzed as the result of the activity of Mt. Remas which plays as the cap rock and andesite breccia with density 2,6 gr/cc.That lithology are being covered by alluvial rock with density 1,9 gr/cc Keyword : gravity method, SVD, modelling, geothermal [Yogyakarta] : Universitas Gadjah Mada 2014 Thesis NonPeerReviewed , MUKHAMAD FARDIAN HATARI SATRIA and , Drs. Imam Suyanto, M.Si. (2014) INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI. UNSPECIFIED thesis, UNSPECIFIED. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=71501
spellingShingle ETD
, MUKHAMAD FARDIAN HATARI SATRIA
, Drs. Imam Suyanto, M.Si.
INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI
title INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI
title_full INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI
title_fullStr INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI
title_full_unstemmed INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI
title_short INTERPRETASI SISTEM PANAS BUMI WAY UMPU MENGGUNAKAN DATA GRAVITASI
title_sort interpretasi sistem panas bumi way umpu menggunakan data gravitasi
topic ETD
work_keys_str_mv AT mukhamadfardianhatarisatria interpretasisistempanasbumiwayumpumenggunakandatagravitasi
AT drsimamsuyantomsi interpretasisistempanasbumiwayumpumenggunakandatagravitasi