<> "The repository administrator has not yet configured an RDF license."^^ . <> . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY"^^ . "Research and data acquisition have been carried out in Pandeglang Regency, \r\nBanten Province. This research uses geomagnetic methods supported by pseudo \r\ngravity transformation and regional geological and local geological data. The \r\ngeomagnetic method is a geophysical method used to measure the total magnetic \r\nfield in a place with the target of obtaining the mineralized zone in the study area. \r\nThe geology of the research area is dominated by volcanic rocks such as volcanic \r\nandesite, volcanic dacite and tuff in the presence of structural zones and porphyry \r\nintrusion. In the study area, magnetic values of 50.7 to -164 nT with mineralized \r\nareas were estimated to be at a high susceptibility value of 0.003 cgs with depths \r\nreaching 600 meters and pseudo gravity transformation values reaching 2.6 g / \r\ncm3 which are estimated to be igneous rocks associated with igneous rocks \r\nassociated with igneous rocks. alteration minerals. So that the mineralized zone is \r\nobtained from the southeast to northwest with a depth of 600 meters around the \r\nstructure zone and there are 4 recommended drill points from the 3D inversion \r\nresults.\r\nKeywords: mineralization, Geomagnetic, Pseudo gravity.\r\n\r\n\r\nResearch and data acquisition have been carried out in Pandeglang Regency, \r\nBanten Province. This research uses geomagnetic methods supported by pseudo \r\ngravity transformation and regional geological and local geological data. The \r\ngeomagnetic method is a geophysical method used to measure the total magnetic \r\nfield in a place with the target of obtaining the mineralized zone in the study area. \r\nThe geology of the research area is dominated by volcanic rocks such as volcanic \r\nandesite, volcanic dacite and tuff in the presence of structural zones and porphyry \r\nintrusion. In the study area, magnetic values of 50.7 to -164 nT with mineralized \r\nareas were estimated to be at a high susceptibility value of 0.003 cgs with depths \r\nreaching 600 meters and pseudo gravity transformation values reaching 2.6 g / \r\ncm3 which are estimated to be igneous rocks associated with igneous rocks \r\nassociated with igneous rocks. alteration minerals. So that the mineralized zone is \r\nobtained from the southeast to northwest with a depth of 600 meters around the \r\nstructure zone and there are 4 recommended drill points from the 3D inversion \r\nresults.\r\nKeywords: mineralization, Geomagnetic, Pseudo gravity."^^ . "2019-11-11" . . . . . "Fakultas Teknik"^^ . . . . . . . "1515051038"^^ . "Angga Reza Yuzi Panitin"^^ . "1515051038 Angga Reza Yuzi Panitin"^^ . . . . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (File PDF)"^^ . . . "ABSTRAK.pdf"^^ . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (File PDF)"^^ . . . "SKRIPSI TANPA BAB PEMBAHASAN.pdf"^^ . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (File PDF)"^^ . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (Other)"^^ . . . . . . "indexcodes.txt"^^ . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (Other)"^^ . . . . . . "indexcodes.txt"^^ . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (Other)"^^ . . . . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (Other)"^^ . . . . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (Other)"^^ . . . . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (Other)"^^ . . . . . . "IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN\r\nINVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY (Other)"^^ . . . . . . 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