creators_name: Angga Reza Yuzi Panitin, 1515051038
creators_id: -
type: other
datestamp: 2022-03-29 13:33:34
lastmod: 2022-03-29 13:33:34
metadata_visibility: show
title: IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN
INVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY
ispublished: pub
subjects: 600
full_text_status: restricted
abstract: 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.
date: 2019-11-11
date_type: published
publisher: Fakultas Teknik
place_of_pub: Universitas Lampung
citation:   Angga Reza Yuzi Panitin, 1515051038  (2019) IDENTIFIKASI ZONA MINERALISASI BERDASARKAN PEMODELAN INVERSI 3D DATA ANOMALI MAGNETIK SERTA PSEUDO GRAVITY.  Fakultas Teknik, Universitas Lampung.     
document_url: http://digilib.unila.ac.id/56617/1/ABSTRAK.pdf
document_url: http://digilib.unila.ac.id/56617/2/SKRIPSI%20TANPA%20BAB%20PEMBAHASAN.pdf
document_url: http://digilib.unila.ac.id/56617/3/SKRIPSI%20FULL.pdf