TY  - THES
N1  - Nugroho Budi Wibowo, M.Si,
ID  - digilib16514
UR  - https://digilib.uin-suka.ac.id/id/eprint/16514/
A1  - EKA PURWITA SARI, NIM. 11620015
Y1  - 2015/06/23/
N2  - Geoelectric measurements have been carried out around the geothermal
manifestations Parangwedang, Yogyakarta, which aims to determine the structure
of the subsurface and the depth of the aquifer based on the value of resistivity (?)
and temperature wells. Data collection was performed by using Syscal on a 4
point measurement with Schlumberger and 2 line configuration with a dipoledipole
configuration. Measurement data were analyzed by two-dimensional
modeling software RES2DINV to obtain resistivity values. Based on the results of
the study, after the data is processed using software and software RES2DINV
Progress obtained rock layers namely: At the top of the ground up at a depth of 0
to 1.71 m is topsoil (overburden) with a value of ? (785 ?m) is a sandy dunes.
From the depths of 1,71- 5,13 m with a value of ? (381- 785 ?m) is a layer of
sandy clay. From the depths of 5.13 to 8.72 m with a value of ? (43,7- 186 ?m)
interpreted as sandstone and interpreted as a layer that can serve to store and drain
the water, the aquifer could be called just that this aquifer is shallow to hold water
surface. From a depth of 12.7 m with a value 5,72- ? (5,02- 21.3 ?m) is an aquifer
system that contains a lot of water. Shallow aquifer located at a depth of 5.27 to
12.8 meters. Smur temperature data about the geothermal manifestations
classified as moderate temperature.
PB  - UIN SUNAN KALIJAGA YOGYAKARTA
KW  - Geoelectric
KW  -  resistivity
KW  -  Manifestation of Geothermal
M1  - skripsi
TI  - INTERPRETASI LAPISAN BATUAN BAWAH PERMUKAAN DI SEKITAR MANIFESTASI PANAS BUMI PARANGWEDANG KABUPATEN BANTUL
YOGYAKARTA BERDASARKAN PENGUKURAN GEOLISTRIK DENGAN METODE RESISTIVITAS
AV  - restricted
EP  - 95
ER  -