Open AccessDetermination of Geological Strike Based on Magnetotelluric’s Polar Diagram and Geological Condition in Tangkuban Parahu’s Geothermal Area
Author(s) -
Muhammad Hafidz,
Wahyu Srigutomo,
Rachmat Sule
Publication year - 2019
Publication title -
iop conference series. earth and environmental science
Language(s) - English
Resource type - Journals
eISSN - 1755-1307
pISSN - 1755-1315
DOI - 10.1088/1755-1315/318/1/012047
Subject(s) - magnetotellurics , geology , geothermal gradient , lineament , geothermal exploration , inversion (geology) , seismology , diagram , geophysics , volcano , polar , tectonics , geologic map , geothermal energy , geomorphology , electrical resistivity and conductivity , statistics , physics , mathematics , astronomy , electrical engineering , engineering
In geothermal exploration, magnetotelluric method (MT) has the capability to resolve conductive body which then can be interpreted as cap rock. A reliable representation of the Earth’s resistivity dimensionality can be achieved by incorporating the direction of geoelectrical strike and geological condition in the geothermal area. In this study, the magnetotelluric method was applied in Tangkuban Parahu volcanic area to reveal the subsurface structure of the area. Due to the uncertainty of MT modelling result, dimensionality analysis (polar diagram) is performed to find out MT data characteristic prior to MT inversion modelling. After that, lineament is mapped based on elevation map to estimate geological strike. Both methods are validated by geological condition in Tangkuban Parahu. The result of polar diagram analysis shows that the direction of geoelectrical strike is dominated NE-SW in mostly frequency and the result of lineament shows similar direction with polar diagram analysis as plotted in rose diagram yields about N45°E.