@phdthesis{digilib69978,
           month = {January},
           title = {ANALISIS BIDANG GELINCIR DENGAN METODE GEOLISTRIK KONFIGURASI DIPOLE-DIPOLE DI DUSUN BENGLE, KECAMATAN TIRTOMOYO, KABUPATEN WONOGIRI},
          school = {UIN SUNAN KALIJAGA YOGYAKARTA},
          author = {NIM.: 21106020026 Indar Mery Sulya Aryani},
            year = {2025},
            note = {Dr. Taqibul Fikri Niyartama, S.Si., M.Si. dan Nugroho Budi Wibowo, S.Si., M.Sc},
        keywords = {Tanah longsor, Bidang Gelincir, Metode Geolistrik, Konfigurasi Dipole-Dipole},
             url = {https://digilib.uin-suka.ac.id/id/eprint/69978/},
        abstract = {The landslide disaster that occurred in Bengle Hamlet, Dlepih Village, Tirtomoyo District, Wonogiri Regency has resulted in two fatalities and damage to several houses. The factor that influences the occurrence of landslides is the presence of slip areas. The slip area can be identified by identifying subsurface layers using geophysical methods. The method used in this research is the geoelectric resistivity method with a resistivity meter, namely the Naniura NRD-300 HF and produces current and potential difference values. The resulting data is then processed using Res2dinv software. From the processing results, it was obtained that the resistivity value range for the area was 2.32 to 3803 ?m. classified into two categories, namely, values {$\leq$}107 ?m are sediment deposits that act as landslide material. Values {\ensuremath{>}}107 ?m are included in the bedrock category which acts as a slip surface. The slip area is thought to be andesite which stretches from west to east with a thickness of {$\pm$} 17 meters.}
}