%0 Generic
%A Angga Reza Yuzi Panitin, 1515051038
%C Universitas Lampung
%D 2019
%F eprints:56617
%I Fakultas Teknik
%T IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN  INVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY
%U http://digilib.unila.ac.id/56617/
%X Research and data acquisition have been carried out in Pandeglang Regency,   Banten Province. This research uses geomagnetic methods supported by pseudo   gravity transformation and regional geological and local geological data. The   geomagnetic method is a geophysical method used to measure the total magnetic   field in a place with the target of obtaining the mineralized zone in the study area.   The geology of the research area is dominated by volcanic rocks such as volcanic   andesite, volcanic dacite and tuff in the presence of structural zones and porphyry   intrusion. In the study area, magnetic values of 50.7 to -164 nT with mineralized   areas were estimated to be at a high susceptibility value of 0.003 cgs with depths   reaching 600 meters and pseudo gravity transformation values reaching 2.6 g /   cm3 which are estimated to be igneous rocks associated with igneous rocks   associated with igneous rocks. alteration minerals. So that the mineralized zone is   obtained from the southeast to northwest with a depth of 600 meters around the   structure zone and there are 4 recommended drill points from the 3D inversion   results.  Keywords: mineralization, Geomagnetic, Pseudo gravity.      Research and data acquisition have been carried out in Pandeglang Regency,   Banten Province. This research uses geomagnetic methods supported by pseudo   gravity transformation and regional geological and local geological data. The   geomagnetic method is a geophysical method used to measure the total magnetic   field in a place with the target of obtaining the mineralized zone in the study area.   The geology of the research area is dominated by volcanic rocks such as volcanic   andesite, volcanic dacite and tuff in the presence of structural zones and porphyry   intrusion. In the study area, magnetic values of 50.7 to -164 nT with mineralized   areas were estimated to be at a high susceptibility value of 0.003 cgs with depths   reaching 600 meters and pseudo gravity transformation values reaching 2.6 g /   cm3 which are estimated to be igneous rocks associated with igneous rocks   associated with igneous rocks. alteration minerals. So that the mineralized zone is   obtained from the southeast to northwest with a depth of 600 meters around the   structure zone and there are 4 recommended drill points from the 3D inversion   results.  Keywords: mineralization, Geomagnetic, Pseudo gravity.