PEMETAAN SEBARAN BATUAN PENYUSUN PAGAR CANDI DI SITUS CANDI LOSARI DUSUN LOSARI, DESA SALAM, KECAMATAN SALAM, KABUPATEN MAGELANG BERDASARKAN METODE MAGNETIK

Main Authors: Ariani, Novi Dwi, Niyartama, Thaqibul Fikri, Wibowo, Nugroho Budi
Format: Article info Map application/pdf Journal
Bahasa: ind
Terbitan: Balai Arkeologi Yogyakarta , 2013
Subjects:
Online Access: http://berkalaarkeologi.kemdikbud.go.id/index.php/berkalaarkeologi/article/view/10
http://berkalaarkeologi.kemdikbud.go.id/index.php/berkalaarkeologi/article/view/10/21
ctrlnum article-10
fullrecord <?xml version="1.0"?> <dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><title lang="en-US">PEMETAAN SEBARAN BATUAN PENYUSUN PAGAR CANDI DI SITUS CANDI LOSARI DUSUN LOSARI, DESA SALAM, KECAMATAN SALAM, KABUPATEN MAGELANG BERDASARKAN METODE MAGNETIK</title><title lang="id-ID">PEMETAAN SEBARAN BATUAN PENYUSUN PAGAR CANDI DI SITUS CANDI LOSARI DUSUN LOSARI, DESA SALAM, KECAMATAN SALAM, KABUPATEN MAGELANG BERDASARKAN METODE MAGNETIK</title><creator>Ariani, Novi Dwi</creator><creator>Niyartama, Thaqibul Fikri</creator><creator>Wibowo, Nugroho Budi</creator><subject lang="en-US">Proton Precession Magnetometer (PPM)</subject><subject lang="en-US">Anomaly</subject><subject lang="en-US">succeptibility</subject><subject lang="en-US">losari temple</subject><subject lang="en-US">Suseptibilitas</subject><subject lang="en-US">Archaeology</subject><subject lang="id-ID">Proton Precession Magnetometer (PPM)</subject><subject lang="id-ID">Anomali</subject><subject lang="id-ID">Suseptibilitas</subject><description lang="en-US">Mapping geophysics research was conducted by geomagnetic method to know anomaly pattern of magnetic pole and to know distribution location and depth of temple gate composing stone in Losari Temple Site by using magnetic data. Data collection used Proton Precessions Magnetometer (PPM) G-856AX by area width of 88 km x 40 km and measurement space of 3 meter used looping method. Field data was corrected by daily variation and IGRF (International Geomagnetics Reference Field) correction and then reduction to pole. The slice modeling was conducted on local anomaly map on height of 6 meter. The result of the local magnetic field anomalies incision then interpolated to get an idea of the spread and depth of rocks making up the fence Losari temple. Local anomaly map shows that anomaly position lies in southwest, southeast, and northeast from main temple. Based from interpolated distribution of magnetic pole anomaly is dominated in depth of 2 meter to 4 meter.&#xA0;</description><description lang="id-ID">Pemetaan geofisika dengan metode geomagnetik dilakukan untuk mengetahui&#xA0;pola anomali kutub magnet serta untuk mengetahui letak sebaran dan kedalaman batu&#xA0;batuan penyusun pagar candi di situs Candi Losari dengan menggunakan data magnetik.&#xA0;Pengambilan data menggunakan Proton Precessions Magnetometer (PPM) G-856AX&#xA0;dengan luas area dari 88 km x 40 km dan spasi pengukuran 3 meter menggunakan&#xA0;metode looping. Data lapangan dilakukan koreksi variasi harian dan IGRF (International&#xA0;Geomagnetics Reference Field) dan kemudian direduksi ke kutub. Pemodelan sayatan&#xA0;dilakukan pada peta anomali lokal ketinggian 6 meter. Hasil sayatan medan magnet&#xA0;anomali lokal kemudian diinterpolasi untuk mendapatkan gambaran sebaran serta&#xA0;kedalaman batuan penyusun pagar candi Losari. Peta anomali lokal menunjukkan bahwa&#xA0;posisi anomali target terletak di barat daya, tenggara, dan timur laut dari candi utama.&#xA0;Berdasarkan dari penyebaran interpolasi anomali kutub magnet didominasi di kedalaman&#xA0;2 meter sampai 4 meter.&#xA0;</description><publisher lang="en-US">Balai Arkeologi Yogyakarta</publisher><date>2013-05-31</date><type>Journal:Article</type><type>Other:info:eu-repo/semantics/publishedVersion</type><type>Journal:Article</type><type>Map:Map</type><type>File:application/pdf</type><identifier>http://berkalaarkeologi.kemdikbud.go.id/index.php/berkalaarkeologi/article/view/10</identifier><identifier>10.30883/jba.v33i1.10</identifier><source lang="en-US">Berkala Arkeologi; Vol. 33 No. 1 (2013); 121-131</source><source>2548-7132</source><source>0216-1419</source><language>ind</language><relation>http://berkalaarkeologi.kemdikbud.go.id/index.php/berkalaarkeologi/article/view/10/21</relation><rights lang="en-US">Copyright (c) 2013 Berkala Arkeologi</rights><recordID>article-10</recordID></dc>
language ind
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author Ariani, Novi Dwi
Niyartama, Thaqibul Fikri
Wibowo, Nugroho Budi
title PEMETAAN SEBARAN BATUAN PENYUSUN PAGAR CANDI DI SITUS CANDI LOSARI DUSUN LOSARI, DESA SALAM, KECAMATAN SALAM, KABUPATEN MAGELANG BERDASARKAN METODE MAGNETIK
publisher Balai Arkeologi Yogyakarta
publishDate 2013
topic Proton Precession Magnetometer (PPM)
Anomaly
succeptibility
losari temple
Suseptibilitas
Archaeology
Anomali
url http://berkalaarkeologi.kemdikbud.go.id/index.php/berkalaarkeologi/article/view/10
http://berkalaarkeologi.kemdikbud.go.id/index.php/berkalaarkeologi/article/view/10/21
contents Mapping geophysics research was conducted by geomagnetic method to know anomaly pattern of magnetic pole and to know distribution location and depth of temple gate composing stone in Losari Temple Site by using magnetic data. Data collection used Proton Precessions Magnetometer (PPM) G-856AX by area width of 88 km x 40 km and measurement space of 3 meter used looping method. Field data was corrected by daily variation and IGRF (International Geomagnetics Reference Field) correction and then reduction to pole. The slice modeling was conducted on local anomaly map on height of 6 meter. The result of the local magnetic field anomalies incision then interpolated to get an idea of the spread and depth of rocks making up the fence Losari temple. Local anomaly map shows that anomaly position lies in southwest, southeast, and northeast from main temple. Based from interpolated distribution of magnetic pole anomaly is dominated in depth of 2 meter to 4 meter.
Pemetaan geofisika dengan metode geomagnetik dilakukan untuk mengetahui pola anomali kutub magnet serta untuk mengetahui letak sebaran dan kedalaman batu batuan penyusun pagar candi di situs Candi Losari dengan menggunakan data magnetik. Pengambilan data menggunakan Proton Precessions Magnetometer (PPM) G-856AX dengan luas area dari 88 km x 40 km dan spasi pengukuran 3 meter menggunakan metode looping. Data lapangan dilakukan koreksi variasi harian dan IGRF (International Geomagnetics Reference Field) dan kemudian direduksi ke kutub. Pemodelan sayatan dilakukan pada peta anomali lokal ketinggian 6 meter. Hasil sayatan medan magnet anomali lokal kemudian diinterpolasi untuk mendapatkan gambaran sebaran serta kedalaman batuan penyusun pagar candi Losari. Peta anomali lokal menunjukkan bahwa posisi anomali target terletak di barat daya, tenggara, dan timur laut dari candi utama. Berdasarkan dari penyebaran interpolasi anomali kutub magnet didominasi di kedalaman 2 meter sampai 4 meter.
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