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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
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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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>
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APA 7
Rasimeng, S., Sianturi, R. J., Surbakti, L. D., Kurniawan, Y., Dani, I., & Rustadi, R. (2024). 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, 13(1), 45–55. https://doi.org/10.24042/jipfalbiruni.v13i1.18555
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IEEE
S. Rasimeng, R. J. Sianturi, L. D. Surbakti, Y. Kurniawan, I. Dani, and R. Rustadi, “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, pp. 45–55, 2024, doi: 10.24042/jipfalbiruni.v13i1.18555.
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