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        <dc:title>ANALISIS DUGAAN JALUR SESAR LOKAL MENGGUNAKAN METODE MIKROTREMOR DI DESA TOTOGAN, KECAMATAN KARANGSAMBUNG, KABUPATEN KEBUMEN</dc:title>
        <dc:creator>Muhammad Faza Syaddad Ar-Rafi, NIM.: 22106020023</dc:creator>
        <dc:subject>530 Fisika</dc:subject>
        <dc:description>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.</dc:description>
        <dc:date>2026-07-08</dc:date>
        <dc:type>Thesis</dc:type>
        <dc:type>NonPeerReviewed</dc:type>
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        <dc:identifier>https://digilib.uin-suka.ac.id/id/eprint/78707/1/22106020023_BAB-I_IV-atau-V_DAFTAR-PUSTAKA.pdf</dc:identifier>
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        <dc:language>id</dc:language>
        <dc:identifier>https://digilib.uin-suka.ac.id/id/eprint/78707/2/22106020023_BAB-II_sampai_SEBELUM-BAB-TERAKHIR.pdf</dc:identifier>
        <dc:identifier>  Muhammad Faza Syaddad Ar-Rafi, NIM.: 22106020023  (2026) ANALISIS DUGAAN JALUR SESAR LOKAL MENGGUNAKAN METODE MIKROTREMOR DI DESA TOTOGAN, KECAMATAN KARANGSAMBUNG, KABUPATEN KEBUMEN.  Skripsi thesis, UIN SUNAN KALIJAGA YOGYAKARTA.   </dc:identifier></oai_dc:dc>
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