HYDROGEOCHEMICAL INVESTIGATION OF ORTAKÇI HOT AND MINERALIZED SPRING (BUHARKENT-AYDIN)
The temperature and discharge of the Ortakçı hot and mineralized water are 48.1 °C and 2.4 l/s, respectively. The spring has being formed as a result of ascending geothermal fluid due to the tectonic activity of the region. The geothermal fluid within joints has not been reached to chemical equilibr...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Pamukkale University
2005-02-01
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| Series: | Pamukkale University Journal of Engineering Sciences |
| Subjects: | |
| Online Access: | http://dergipark.ulakbim.gov.tr/pajes/article/view/5000089483 |