@phdthesis{digilib32103,
           month = {May},
           title = {IDENTIFIKASI LAPISAN TANAH RAWAN LONGSOR
MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI WENNER
DI DESA GAYAMHARJO KECAMATAN PRAMBANAN KABUPATEN
SLEMAN},
          school = {UIN SUNAN KALIJAGA YOGYAKARTA},
          author = {NIM. 13620034 NAJILA TIHURUA},
            year = {2018},
            note = {Dr. Thaqibul Fikri Niyartama, M.Si},
        keywords = {Prambanan, Resistivity, and Landslide},
             url = {https://digilib.uin-suka.ac.id/id/eprint/32103/},
        abstract = {Landslides occur due to the field of slip. Identification of Soil Landslide
Identification Using Geolistrik Method The Wenner configuration has been
done in Gayamharjo Village, Prambanan Sub-district, Sleman District. This
study aims to determine the structure of subsurface rocks and identify the field
of ground slip in the landslide prone areas in the study area. Measurements
were made as many as 3 trajectories, the smallest spaced between 20 meters
electrode with 300 meters of track length. The tool used is Syscal Jr Switch-48.
Data processing uses RES2DINV software that produces 2D subsurface
modeling. The results of the interpretation showed that the location of the study
identified the constituent rock consisting of three layers of subsurface rocks
(1,36 to 6,86) ?m, sandstone (15,4 to 34,6) ?m, and andesite rocks (77, 8 to
393) ?m. In the three trajectories of the research area, there is a slip field with
the potential for landslide: track 1 at point 40 s.d.80 with a depth of 37 m, track
2 at point 220 s.d. 240 with depth 26 m, path 3 at point 100 s.d. 140 with a
depth of 37 m.}
}