TY  - THES
N1  - Dr. Thaqibul Fikri Niyartama, S.Si., M.Si. dan Dr. Nugroho Budi Wibowo, S.Si., M.Si.
ID  - digilib75895
UR  - https://digilib.uin-suka.ac.id/id/eprint/75895/
A1  - Muhammad Habib Qaulan Shadida, NIM.: 22106020026
Y1  - 2026/01/15/
N2  - This research was conducted in a landslide area characterized by soil creep in Deot
Hamlet, Totogan Village, Karangsambung District, Kebumen. The study aims to
analyze subsurface ground density profiles to identify rock types within the
landslide zone using the ellipticity curve method and to assess landslide potential.
Data were acquired using the microtremor method at 17 measurement points with
intervals of approximately ±50 meters. The study area is located within the
coordinate boundaries of 109° 40' 35.9'' E to 109° 46' 3'' E and 7° 31' 09.2'' S to 7°
31' 12.5'' S, and is composed of Schist and Phyllite Formations. The recorded
microtremor signals were filtered to remove noise and processed using the HVSR
(Horizontal to Vertical Spectral Ratio) method to obtain HVSR curves, which were
then used as input for the ellipticity curve method to estimate density values and
their corresponding depths. The results show that density values of < 1764 kg/m³
represent surface soil, 1764?2243 kg/m³ correspond to clay, 2244?2800 kg/m³
indicate phyllite, and > 2800 kg/m³ represent schist. The identified ground
movement type is soil creep, caused by the bedrock slope dipping in the same
direction as the surface slope of the study area. The study also delineates two
landslide zones: non-affected and non-potential zones, and affected and potentially
unstable zones.
PB  - UIN SUNAN KALIJAGA YOGYAKARTA
KW  - Mikrotremor
KW  -  Densitas
KW  -  HVSR
KW  -  Ellipticity Curve
KW  -  Rayapan
KW  - 
Karangsambung
M1  - skripsi
TI  - ANALISIS JENIS BATUAN PADA ZONA GERAKAN TANAH MENGGUNAKAN METODE MIKROTREMOR DI DUSUN DEOT, DESA TOTOGAN, KECAMATAN KARANGSAMBUNG, KEBUMEN
AV  - restricted
EP  - 108
ER  -