Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik
Abstract Acquisition of geomagnetic field has been done at Kretek, Sanden, Pundong, Bantul and Panggang, Gunung Kidul, Yogjakarta Province on 14 s/d 17 October and 7,8,9,12 November 2009 in orde to interpreted the subsurface structure. Data has been collected by Proton Precession Magnetometer (PPM)...
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BERKALA FISIKA
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ftundipojs:oai:ojs.ejournal.undip.ac.id:article/2924 2024-09-09T19:58:41+00:00 Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik Indratmoko, Putut Nurwidyanto, M. Irham Yulianto, Tony 2012-03-29 application/pdf https://ejournal.undip.ac.id/index.php/berkala_fisika/article/view/2924 eng eng BERKALA FISIKA https://ejournal.undip.ac.id/index.php/berkala_fisika/article/view/2924/2612 https://ejournal.undip.ac.id/index.php/berkala_fisika/article/view/2924 BERKALA FISIKA; Vol 12, No 4 (2009): Berkala Fisika; 153-160 1410-9662 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2012 ftundipojs 2024-06-20T03:48:27Z Abstract Acquisition of geomagnetic field has been done at Kretek, Sanden, Pundong, Bantul and Panggang, Gunung Kidul, Yogjakarta Province on 14 s/d 17 October and 7,8,9,12 November 2009 in orde to interpreted the subsurface structure. Data has been collected by Proton Precession Magnetometer (PPM) to measured the total intensity of magnetic field, Global Positioning System (GPS) to determine the position and geology compass to the direction of north pole. The raw data has been processed and performed using IGRF (International Geomagnetics Reference Field) correction to obtain total field magnetic anomaly. Upward continuation was performed at 300 meters heigh by Magpick. Qualitative interpretation was done by analyzing regional and local anomaly maps. Quantitative interpretation was done 2 ½ D modelling cross-sectionanomaly maps using Mag2DC for Windows Software. The result of 2-D modeling produces anomaly objects was susceptibility value (0,0405) in cgs unit for the first object, susceptibility value (0,0425) in cgs unit for the second object, susceptibility value (-0,0085) in cgs unit for the third object. The anomaly objects had depth in +580 meters from the surface and was considered the rock which had been experience demagnetitation proses. Key word: magnetic anomaly, Parangtritis, susceptibilities. Article in Journal/Newspaper North Pole Universitas Diponegoro: Undip E-Journal System (UEJS) Portal North Pole Sanden ENVELOPE(8.086,8.086,62.889,62.889) |
institution |
Open Polar |
collection |
Universitas Diponegoro: Undip E-Journal System (UEJS) Portal |
op_collection_id |
ftundipojs |
language |
English |
description |
Abstract Acquisition of geomagnetic field has been done at Kretek, Sanden, Pundong, Bantul and Panggang, Gunung Kidul, Yogjakarta Province on 14 s/d 17 October and 7,8,9,12 November 2009 in orde to interpreted the subsurface structure. Data has been collected by Proton Precession Magnetometer (PPM) to measured the total intensity of magnetic field, Global Positioning System (GPS) to determine the position and geology compass to the direction of north pole. The raw data has been processed and performed using IGRF (International Geomagnetics Reference Field) correction to obtain total field magnetic anomaly. Upward continuation was performed at 300 meters heigh by Magpick. Qualitative interpretation was done by analyzing regional and local anomaly maps. Quantitative interpretation was done 2 ½ D modelling cross-sectionanomaly maps using Mag2DC for Windows Software. The result of 2-D modeling produces anomaly objects was susceptibility value (0,0405) in cgs unit for the first object, susceptibility value (0,0425) in cgs unit for the second object, susceptibility value (-0,0085) in cgs unit for the third object. The anomaly objects had depth in +580 meters from the surface and was considered the rock which had been experience demagnetitation proses. Key word: magnetic anomaly, Parangtritis, susceptibilities. |
format |
Article in Journal/Newspaper |
author |
Indratmoko, Putut Nurwidyanto, M. Irham Yulianto, Tony |
spellingShingle |
Indratmoko, Putut Nurwidyanto, M. Irham Yulianto, Tony Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik |
author_facet |
Indratmoko, Putut Nurwidyanto, M. Irham Yulianto, Tony |
author_sort |
Indratmoko, Putut |
title |
Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik |
title_short |
Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik |
title_full |
Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik |
title_fullStr |
Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik |
title_full_unstemmed |
Interpretasi Bawah Permukaan Daerah Manifestasi Panas Bumi Parang Tritis Kabupaten Bantul DIY Dengan Metode Magnetik |
title_sort |
interpretasi bawah permukaan daerah manifestasi panas bumi parang tritis kabupaten bantul diy dengan metode magnetik |
publisher |
BERKALA FISIKA |
publishDate |
2012 |
url |
https://ejournal.undip.ac.id/index.php/berkala_fisika/article/view/2924 |
long_lat |
ENVELOPE(8.086,8.086,62.889,62.889) |
geographic |
North Pole Sanden |
geographic_facet |
North Pole Sanden |
genre |
North Pole |
genre_facet |
North Pole |
op_source |
BERKALA FISIKA; Vol 12, No 4 (2009): Berkala Fisika; 153-160 1410-9662 |
op_relation |
https://ejournal.undip.ac.id/index.php/berkala_fisika/article/view/2924/2612 https://ejournal.undip.ac.id/index.php/berkala_fisika/article/view/2924 |
_version_ |
1809929724363800576 |