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bibo:abstract "The suspected presence of a local fault in Totogan Village, Karangsambung\r\nSubdistrict, Kebumen Regency, is believed to play a role in controlling subsurface\r\ngeological conditions and soil dynamic characteristics in the study area. This\r\nstudy aims to identify wave source direction patterns based on H/V rotate analysis\r\nand to analyze the distribution of shear wave velocity (vs) as an indicator of the\r\npresence of geological structural zones. The methods used were microtremors\r\nwith Horizontal to Vertical Spectral Ratio (HVSR) analysis and H/V rotate to\r\nobtain wave source direction patterns. The processed data were then used to\r\nconstruct a vs distribution model visualized in the form of a solid model and a\r\nsolid fence diagram. Additionally, supporting data analysis, including lineaments\r\nand Fault Fracture Density (FFD), was conducted to strengthen the\r\ninterpretation of subsurface geological structures. The results of the study\r\nindicate that the dominant direction of the wave source tends to be North–South,\r\nwith an average azimuth of N 4.6° E, as well as several other directions such as\r\nEast–West and Northeast–Southwest. The shear wave velocity (vs) values range\r\nfrom 153.03 m/s to 1495.90 m/s. Zones with vs values > 1200 m/s are found in the\r\nC–C’ section in the Northern part and again in the A–A’ section in the Southern\r\npart with a Northeast–Southwest orientation. Additionally, zones with vs values <\r\n500 m/s were identified, appearing in the Western part of the study area along the\r\nB–B’ section and reappearing in the Eastern part along the E–E’ section with an\r\nEast–West orientation. The results of integrating all methods indicate the\r\npresence of local fault zones influenced by the geological structure in the study\r\narea."^^xsd:string;
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dc:title "HTML Summary of #78707 \n\nANALISIS DUGAAN JALUR SESAR LOKAL MENGGUNAKAN METODE MIKROTREMOR DI DESA TOTOGAN, KECAMATAN KARANGSAMBUNG, KABUPATEN KEBUMEN\n\n";
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