<mets:mets OBJID="eprint_78707" 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="2026-10-08T01:50:34Z"><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_78707_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:titleInfo><mods:title>ANALISIS DUGAAN JALUR SESAR LOKAL MENGGUNAKAN METODE MIKROTREMOR DI DESA TOTOGAN, KECAMATAN KARANGSAMBUNG, KABUPATEN KEBUMEN</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">NIM.: 22106020023</mods:namePart><mods:namePart type="family">Muhammad Faza Syaddad Ar-Rafi</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>The suspected presence of a local fault in Totogan Village, Karangsambung&#13;
Subdistrict, Kebumen Regency, is believed to play a role in controlling subsurface&#13;
geological conditions and soil dynamic characteristics in the study area. This&#13;
study aims to identify wave source direction patterns based on H/V rotate analysis&#13;
and to analyze the distribution of shear wave velocity (vs) as an indicator of the&#13;
presence of geological structural zones. The methods used were microtremors&#13;
with Horizontal to Vertical Spectral Ratio (HVSR) analysis and H/V rotate to&#13;
obtain wave source direction patterns. The processed data were then used to&#13;
construct a vs distribution model visualized in the form of a solid model and a&#13;
solid fence diagram. Additionally, supporting data analysis, including lineaments&#13;
and Fault Fracture Density (FFD), was conducted to strengthen the&#13;
interpretation of subsurface geological structures. The results of the study&#13;
indicate that the dominant direction of the wave source tends to be North–South,&#13;
with an average azimuth of N 4.6° E, as well as several other directions such as&#13;
East–West and Northeast–Southwest. The shear wave velocity (vs) values range&#13;
from 153.03 m/s to 1495.90 m/s. Zones with vs values &gt; 1200 m/s are found in the&#13;
C–C’ section in the Northern part and again in the A–A’ section in the Southern&#13;
part with a Northeast–Southwest orientation. Additionally, zones with vs values &lt;&#13;
500 m/s were identified, appearing in the Western part of the study area along the&#13;
B–B’ section and reappearing in the Eastern part along the E–E’ section with an&#13;
East–West orientation. The results of integrating all methods indicate the&#13;
presence of local fault zones influenced by the geological structure in the study&#13;
area.</mods:abstract><mods:classification authority="lcc">530 Fisika</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2026-07-08</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_78707"><mets:rightsMD ID="rights_eprint_78707_mods"><mets:mdWrap MDTYPE="MODS"><mets:xmlData><mods:useAndReproduction>
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