@article{MAKHILLJEAS202015619187,
    title = {Determination of Geothermal using Parameters Resistivity and Phase in the
Two-Dimensional Magnetotelluric Data Modeling Technique in
Central Sulawesi, Bora Area},
    journal = {Journal of Engineering and Applied Sciences},
    volume = {15},
    number = {6},
    pages = {1481-1486},
    year = {2020},
    issn = {1816-949x},
    doi = {jeasci.2020.1481.1486},
    url = {https://makhillpublications.co/view-article.php?issn=1816-949x&doi=jeasci.2020.1481.1486},
    author = {Sunaryo,Tasya,Mutia and},
    keywords = {Magnetotelluric,geothermal,resistivity,TE-TM,SSMT2000,Bora area},
    abstract = {Geophysical research was carried out by using the Magnetotelluric (MT) method on X geothermal
exploration to determine the distribution of resistivity and geothermal reservoir zones. The data included nine
measurement points with TE-TM invariant mode from two-dimensional modeling. Data were processed by
using secondary data from the acquisition process and then utilizing SSMT2000, MTEditor and Win Glink
Software. The results shown in this study were in the form of resistivity and subsequent phases with the
North-South trending geological conditions. From the analysis obtained in the two-dimensional modeling, there
were three distribution zones of resistivity including low, medium and high resistivity distributions. Low
resistivity distribution zones of 4-14 Ωm was estimated to be clay cap, the zone of moderate resistivity
distribution of 19-159 Ωm was estimated to be reservoir rock which controls the appearance of hot water
manifestations and the zone of high resistivity distribution >216 Ωm was estimated to be rock (basement) which
is a geothermal source of the Bora area.}
    }