| dc.contributor.author | Tole, M P | |
| dc.date.accessioned | 2014-07-10T09:16:15Z | |
| dc.date.available | 2014-07-10T09:16:15Z | |
| dc.date.issued | 1985 | |
| dc.identifier.citation | Tole, M. P. (1985). Geochemical studies of the geothermal area east of the Jombo Hill intrusion, Coast Province, Kenya: 1. Hot water reservoir temperatures. | en_US |
| dc.identifier.uri | http://inis.iaea.org/search/search.aspx?orig_q=RN:34005764 | |
| dc.identifier.uri | http://hdl.handle.net/11295/72445 | |
| dc.description.abstract | The hot springs east of Jombo Hill intrusion occur at four different places over an area measuring 9 km x 2 km. They consist of slightly alkaline waters of pH 7.5-8.5, with surface discharge temperatures averaging 59oC - 70oC. Both the silica and the Na-K-Ca geothermometers give temperatures of about 170oC. The minimum temperature for the reservoir therefore is 170oC | en_US |
| dc.language.iso | en | en_US |
| dc.publisher | University of Nairobi | en_US |
| dc.title | Geochemical studies of the geothermal area east of the Jombo Hill intrusion, Coast Province, Kenya: 1. Hot water reservoir temperatures | en_US |
| dc.type | Article | en_US |
| dc.type.material | en | en_US |
