<mods:mods version="3.3" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd" xmlns:mods="http://www.loc.gov/mods/v3" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><mods:titleInfo><mods:title>ANALISIS SEBARAN FORMASI GUNUNGAPI JEMBANGAN DAN KALIBIUK MENGGUNAKAN METODE MAGNETIK DI DESA PENUSUPAN KECAMATAN PEJAWARAN BANJARNEGARA</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">NIM.: 22106020005</mods:namePart><mods:namePart type="family">Adik Tertia Prawanningrum</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>Penusupan Village has a geological setting composed of the Jembangan&#13;
Volcanic Formation (QJYA) and the Kalibiuk Formation (TPB), with varying slope&#13;
gradients and areas affected by ground movement. This study aims to analyze the&#13;
relationship between geological formations and zones suspected to be prone to&#13;
ground movement and to model subsurface conditions based on the interpretation&#13;
of regional magnetic anomalies. Data acquisition was conducted at 49&#13;
measurement points using a Proton Precession Magnetometer (PPM) with an interpoint&#13;
spacing of approximately 130 m. The total magnetic field data were processed&#13;
through diurnal variation correction and International Geomagnetic Reference&#13;
Field (IGRF) correction. The results show that the regional magnetic anomaly&#13;
values range from -147.1 nT to 327.7 nT. Two-dimensional (2D) modeling identified&#13;
the Kalibiuk Formation (TPB) with magnetic susceptibility values of 0.2–0.6 × 10⁻³&#13;
SI at depths of approximately 0–85 m and the Jembangan Volcanic Formation&#13;
(QJYA) with magnetic susceptibility values of 12.0–19.0 × 10⁻³ SI at depths of&#13;
approximately 14–100 m. The zone suspected of experiencing ground movement is&#13;
associated with the Jembangan Volcanic Formation (QJYA) and is located on&#13;
relatively steep slopes. The presence of water seepage within the ground-movement&#13;
zone indicates the influence of hydrological conditions on slope stability.</mods:abstract><mods:classification authority="lcc">530 Fisika</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2026-08-13</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>UIN SUNAN KALIJAGA YOGYAKARTA;FAKULTAS SAINS DAN TEKNOLOGI</mods:publisher></mods:originInfo><mods:genre>Thesis</mods:genre></mods:mods>