Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE Serpong

Experimental Power Reactor (EPR) site is located in Serpong and it has a distance of ± 67 km from the Cimandiri active fault. Result of EPR site evaluation show that it is feasible and safe from the active fault. However, it is necessary to monitor the rock deformation by using Global Positioning Sy...

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Bibliographic Details
Main Authors: Hadi Suntoko, Sriyana
Format: Article
Language:English
Published: Center for Nuclear Minerals Technology 2017-11-01
Series:Eksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir
Subjects:
GPS
Online Access:http://jurnal.batan.go.id/index.php/eksplorium/article/view/3352/pdf
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spelling doaj-cdecc264a3614c67be1bc8af62f3e1e22020-11-24T20:52:28ZengCenter for Nuclear Minerals TechnologyEksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir0854-14182503-426X2017-11-013829910810.17146/eksplorium.2017.38.2.3352Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE SerpongHadi Suntoko0Sriyana 1Pusat Kajian Sistem Energi Nuklir- BATANPusat Kajian Sistem Energi Nuklir- BATANExperimental Power Reactor (EPR) site is located in Serpong and it has a distance of ± 67 km from the Cimandiri active fault. Result of EPR site evaluation show that it is feasible and safe from the active fault. However, it is necessary to monitor the rock deformation by using Global Positioning System(GPS) tool. The goal is to obtain precise coordinates through GPS data to identify the presence of active fault activity and its impact on the site. The monitoring is using six measuring points configuration mounted crossing the southeast-northwest suppose fault line direction. The research method is using coordinate data collection from BATAN GPS periodic station and BIG GPS continuous station in radius 25 km. Data processing is using Bernese Version 5.2 Software, proceed radially from station 1 as reference point and then continued by data interpretation. The Analysis result shows that the fault/tectonic condition near EPR site is in the range of 0.05 microstrain which is an area with stable tectonic condition.http://jurnal.batan.go.id/index.php/eksplorium/article/view/3352/pdfGPSpatahanevaluasi tapakdeformasi
collection DOAJ
language English
format Article
sources DOAJ
author Hadi Suntoko
Sriyana
spellingShingle Hadi Suntoko
Sriyana
Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE Serpong
Eksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir
GPS
patahan
evaluasi tapak
deformasi
author_facet Hadi Suntoko
Sriyana
author_sort Hadi Suntoko
title Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE Serpong
title_short Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE Serpong
title_full Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE Serpong
title_fullStr Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE Serpong
title_full_unstemmed Identifikasi Patahan Menggunakan Analisis Data Deformasi Tanah di Tapak RDE Serpong
title_sort identifikasi patahan menggunakan analisis data deformasi tanah di tapak rde serpong
publisher Center for Nuclear Minerals Technology
series Eksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir
issn 0854-1418
2503-426X
publishDate 2017-11-01
description Experimental Power Reactor (EPR) site is located in Serpong and it has a distance of ± 67 km from the Cimandiri active fault. Result of EPR site evaluation show that it is feasible and safe from the active fault. However, it is necessary to monitor the rock deformation by using Global Positioning System(GPS) tool. The goal is to obtain precise coordinates through GPS data to identify the presence of active fault activity and its impact on the site. The monitoring is using six measuring points configuration mounted crossing the southeast-northwest suppose fault line direction. The research method is using coordinate data collection from BATAN GPS periodic station and BIG GPS continuous station in radius 25 km. Data processing is using Bernese Version 5.2 Software, proceed radially from station 1 as reference point and then continued by data interpretation. The Analysis result shows that the fault/tectonic condition near EPR site is in the range of 0.05 microstrain which is an area with stable tectonic condition.
topic GPS
patahan
evaluasi tapak
deformasi
url http://jurnal.batan.go.id/index.php/eksplorium/article/view/3352/pdf
work_keys_str_mv AT hadisuntoko identifikasipatahanmenggunakananalisisdatadeformasitanahditapakrdeserpong
AT sriyana identifikasipatahanmenggunakananalisisdatadeformasitanahditapakrdeserpong
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