<mets:mets OBJID="eprint_78706" LABEL="Eprints Item" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd" xmlns:mets="http://www.loc.gov/METS/" xmlns:mods="http://www.loc.gov/mods/v3" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><mets:metsHdr CREATEDATE="2026-10-08T01:50:50Z"><mets:agent ROLE="CUSTODIAN" TYPE="ORGANIZATION"><mets:name>Institutional Repository UIN Sunan Kalijaga Yogyakarta</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_eprint_78706_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:titleInfo><mods:title>ANALISIS SUSEPTIBILITAS BATUAN DAN IDENTIFIKASI DUGAAN ZONA SESAR MENGGUNAKAN METODE MAGNETIK DI DESA PENUSUPAN, KECAMATAN PEJAWARAN, KABUPATEN BANJARNEGARA, JAWA TENGAH</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">NIM.: 22106020006</mods:namePart><mods:namePart type="family">Riska Sorayawati</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>This study aims to identify subsurface rock susceptibility values and analyze a&#13;
suspected fault zone in Penusupan Village, Pejawaran District, Banjarnegara Regency.&#13;
Total magnetic field measurements were conducted at 50 points across an area of&#13;
approximately 2.5 km², with a 250-meter interval between points. Magnetic data processing&#13;
involved diurnal variation and IGRF corrections, regional-residual anomaly separation,&#13;
reduction to the pole, upward continuation, Second Vertical Derivative (SVD) and Tilt&#13;
Derivative (TDR) analyses, and 2D subsurface modeling. Modeling results identified four&#13;
lithological units: clayey surface soil (1 – 12) × 10⁻⁵ SI, clay (1 – 2) × 10⁻⁵ SI, sandstone 1&#13;
× 10⁻³ SI, and andesite (1 – 5) × 10⁻² SI. SVD analysis (|MIN| &lt; |MAX|) indicates a&#13;
suspected normal fault with a dominant trend ranging from Northwest–Southeast (135°–&#13;
315°) to West–East (90°–270°). The indirect interpretation of subsurface structures via the&#13;
magnetic method is corroborated by TDR analysis, 2D modeling, and field geological&#13;
validation, which reveal weathering zones and discontinuity planes at the suspected fault&#13;
location.</mods:abstract><mods:classification authority="lcc">530 Fisika</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2026-08-14</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></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_eprint_78706"><mets:rightsMD ID="rights_eprint_78706_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:useAndReproduction>
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    </mods:useAndReproduction></mets:xmlData></mets:mdWrap></mets:rightsMD></mets:amdSec><mets:fileSec><mets:fileGrp USE="reference"><mets:file ID="eprint_78706_1079000_1" SIZE="6016781" OWNERID="https://digilib.uin-suka.ac.id/id/eprint/78706/1/22106020006_BAB-I_IV-atau-V_DAFTAR-PUSTAKA.pdf" MIMETYPE="application/pdf"><mets:FLocat LOCTYPE="URL" xlink:type="simple" xlink:href="https://digilib.uin-suka.ac.id/id/eprint/78706/1/22106020006_BAB-I_IV-atau-V_DAFTAR-PUSTAKA.pdf"></mets:FLocat></mets:file></mets:fileGrp><mets:fileGrp USE="reference"><mets:file ID="eprint_78706_1079001_1" SIZE="11693316" OWNERID="https://digilib.uin-suka.ac.id/id/eprint/78706/2/22106020006_BAB-II_sampai_SEBELUM-BAB-TERAKHIR.pdf" MIMETYPE="application/pdf"><mets:FLocat LOCTYPE="URL" xlink:type="simple" xlink:href="https://digilib.uin-suka.ac.id/id/eprint/78706/2/22106020006_BAB-II_sampai_SEBELUM-BAB-TERAKHIR.pdf"></mets:FLocat></mets:file></mets:fileGrp></mets:fileSec><mets:structMap><mets:div DMDID="DMD_eprint_78706_mods" ADMID="TMD_eprint_78706"><mets:fptr FILEID="eprint_78706_document_1079000_1"></mets:fptr><mets:fptr FILEID="eprint_78706_document_1079001_1"></mets:fptr></mets:div></mets:structMap></mets:mets>