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Estimating Bedrock Depth Based on Total Magnetic Field Anomaly Data in Medan City Area in the Northern Sumatra Basin Using the Peter Half Slope Method

JURNAL ILMIAH PENDIDIKAN FISIKA AL BIRUNI · Vol. 13 No. 1 (2024) · hlm. 45–55

DOI
10.24042/jipfalbiruni.v13i1.18555
ISSN
2503-023X, 2303-1832
Terbit
2024-06-29
Penerbit
Universitas Islam Negeri Raden Intan Lampung, Indonesia
Bahasa
eng

Abstrak

The Peter Half Slope method is valuable for estimating rock depths using total magnetic field anomaly data. It relies on graphical analysis and practical rules to gauge the depths of magnetic sources. This method finds significant utility in magnetic interpretation, measuring half the maximum slope distance on magnetic anomaly curves. The primary objective of this research is to determine anomaly depths within Medan City by applying the Peter Half Slope method. The study employs total magnetic field anomaly data from the Medan city area, a part of the Northern Sumatra Basin. The research methodology includes data preparation, reduction to the pole transformation, profile creation, maximum slope computation, half-slope determination, and identifying tangent points on both minimum and maximum curves. The difference between these tangent points is then calculated to derive the depth of the bedrock. Based on the depth calculations using criteria for very thin, intermediate thickness, and very thick bodies, depths of 401, 301, and 240 meters were obtained, resulting in an average depth of 314 meters. This method plays a pivotal role in characterizing subsurface rock structures and is essential for geophysical analysis and magnetic data interpretation.

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  • Lampung University
  • Hasanuddin University
  • Malikussaleh University
  • University of Bengkulu
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Rekan penulisOrganisasiArtikel bersama
Muhammad NurulLampung University1
Ida Bagus Suananda YogiLampung University1
Aprillia YulianataLampung University1
Aisah YuliantinaLampung University1
Ilham DaniLampung University1
Ambrosius Hernawan WibisonoLampung University1
Restu Wildanu AhadiLampung University1
Sultan Al GhifariLampung University1
Emir Dzakwan Kamal ZeinLampung University1
Egie WijaksonoAfiliasi tidak diketahui1
Fahruddin FahruddinHasanuddin University1
Ferdio ValentinLampung University1
Theressia Githa AuroraLampung University1
Jesica NurlailiLampung University1
Anisa AmandaAfiliasi tidak diketahui1
Rizki Buana AgustianAfiliasi tidak diketahui1
Aksela Dian FistaAfiliasi tidak diketahui1
Muchammad FaridUniversity of Bengkulu1
Nandi HaerudinLampung University1
Deassy SiskaMalikussaleh University1
Helmy FitriawanLampung University1

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Sumber metadata: OAI-PMH (metadata jurnal) http://ejournal.radenintan.ac.id/index.php/al-biruni/oai, pertama di-harvest 9 Nov 2026, terakhir terlihat 9 Nov 2026.
Metadata asli (oai_dc)
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	<dc:title xml:lang="en">Estimating Bedrock Depth Based on Total Magnetic Field Anomaly Data in Medan City Area in the Northern Sumatra Basin Using the Peter Half Slope Method</dc:title>
	<dc:creator xml:lang="en">Rasimeng, Syamsurijal</dc:creator>
	<dc:creator xml:lang="en">Sianturi, Rizky J.</dc:creator>
	<dc:creator xml:lang="en">Surbakti, Lucky Dolinta</dc:creator>
	<dc:creator xml:lang="en">Kurniawan, Yoga</dc:creator>
	<dc:creator xml:lang="en">Dani, Ilham</dc:creator>
	<dc:creator xml:lang="en">Rustadi, Rustadi</dc:creator>
	<dc:subject xml:lang="en">Basin</dc:subject>
	<dc:subject xml:lang="en">Geomagnetic</dc:subject>
	<dc:subject xml:lang="en">Half slope</dc:subject>
	<dc:subject xml:lang="en">Inclination</dc:subject>
	<dc:subject xml:lang="en">Declination</dc:subject>
	<dc:description xml:lang="en">The Peter Half Slope method is valuable for estimating rock depths using total magnetic field anomaly data. It relies on graphical analysis and practical rules to gauge the depths of magnetic sources. This method finds significant utility in magnetic interpretation, measuring half the maximum slope distance on magnetic anomaly curves. The primary objective of this research is to determine anomaly depths within Medan City by applying the Peter Half Slope method. The study employs total magnetic field anomaly data from the Medan city area, a part of the Northern Sumatra Basin. The research methodology includes data preparation, reduction to the pole transformation, profile creation, maximum slope computation, half-slope determination, and identifying tangent points on both minimum and maximum curves. The difference between these tangent points is then calculated to derive the depth of the bedrock. Based on the depth calculations using criteria for very thin, intermediate thickness, and very thick bodies, depths of 401, 301, and 240 meters were obtained, resulting in an average depth of 314 meters. This method plays a pivotal role in characterizing subsurface rock structures and is essential for geophysical analysis and magnetic data interpretation.</dc:description>
	<dc:publisher xml:lang="en">Universitas Islam Negeri Raden Intan Lampung, Indonesia</dc:publisher>
	<dc:date>2024-06-29</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://ejournal.radenintan.ac.id/index.php/al-biruni/article/view/18555</dc:identifier>
	<dc:identifier>10.24042/jipfalbiruni.v13i1.18555</dc:identifier>
	<dc:source xml:lang="en">Jurnal Ilmiah Pendidikan Fisika Al-Biruni; Vol. 13 No. 1 (2024): Jurnal Ilmiah Pendidikan Fisika Al-Biruni; 45-55</dc:source>
	<dc:source xml:lang="id">Jurnal Ilmiah Pendidikan Fisika Al-Biruni; Vol 13 No 1 (2024): Jurnal Ilmiah Pendidikan Fisika Al-Biruni; 45-55</dc:source>
	<dc:source>2503-023X</dc:source>
	<dc:source>2303-1832</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://ejournal.radenintan.ac.id/index.php/al-biruni/article/view/18555/pdf</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2024 Physics Education Department, UIN Raden Intan Lampung, Indonesia</dc:rights>
</oai_dc:dc>