BibTex Citation Data :
@article{YPJ7064, author = {Elvera Yuanita Rukmana and Udi Harmoko}, title = {IDENTIFIKASI PANAS BUMI DIWAK DAN DEREKAN KECAMATAN BERGAS KABUPATEN SEMARANG DENGAN MENGGUNAKAN METODE AUDIOMAGNETOTELLURIK}, journal = {Youngster Physics Journal}, volume = {3}, number = {4}, year = {2014}, keywords = {}, abstract = { Audio-Magnetotellurics (AMT) surveys has been conducted in September 2013 in the Diwak and Derekan geothermal field s . The purpose of the audio-magnetotelluric surveys to indicate heat source, reservoir, and cap rock. The data obtained from the field was apparent resistivity, phase difference, and coherence as a function of frequency are processed using softwere package WinGLink then matched with regional geological information studies, and the results are interpreted. Characterization of geothermal systems include the caprock with a resistivity of 0-10Ωm value where the area is a zone of conductivity . Then the reservoir area is suspected to have a resistivity value with arange of 50-500 Ωm with a depth of about 500 m . In the heat source located in a geothermal system resistivity values > 500Ωm w ith a depth of about 1.5 km . Keywords: AMT, geothermal, resistivity }, issn = {2302-7371}, pages = {267--270} url = {https://ejournal3.undip.ac.id/index.php/bfd/article/view/7064} }
Refworks Citation Data :
Audio-Magnetotellurics (AMT) surveys has been conducted in September 2013 in the Diwak and Derekan geothermal fields. The purpose of the audio-magnetotelluric surveys to indicate heat source, reservoir, and cap rock.
The data obtained from the field was apparent resistivity, phase difference, and coherence as a function of frequency are processed using softwere package WinGLink then matched with regional geological information studies, and the results are interpreted.
Characterization of geothermal systems include the caprock with a resistivity of 0-10Ωm value where the area is a zone of conductivity. Then the reservoir area is suspected to have a resistivity value with arange of 50-500 Ωm with a depth of about 500 m. In the heat source located in a geothermal system resistivity values > 500Ωm with a depth of about 1.5 km.
Keywords: AMT, geothermal, resistivity
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