| dc.contributor.author |
Gartzos, E |
en |
| dc.contributor.author |
Stamatis, G |
en |
| dc.date.accessioned |
2014-06-06T06:43:02Z |
|
| dc.date.available |
2014-06-06T06:43:02Z |
|
| dc.date.issued |
1996 |
en |
| dc.identifier.issn |
00283630 |
en |
| dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/965 |
|
| dc.relation.uri |
http://www.scopus.com/inward/record.url?eid=2-s2.0-0342995339&partnerID=40&md5=2465afce467293928f6b619c04312593 |
en |
| dc.title |
Genesis of the thermal springs of the Sperchios graben, Greece |
en |
| heal.type |
journalArticle |
en |
| heal.publicationDate |
1996 |
en |
| heal.abstract |
The western branch of the active volcanic island arc of Greece extends up to the Maliakos gulf and intersects the eastern extention of the Sperchios graben. The volcanic activity offers the required thermal energy for the heating of the deep circulating waters and their ascend to the surface. The deep water circulation follows the channelways formed by the active faults and the associated fracture zones. The thermal springs occurring at the southern margin of the Sperchios graben are closer to the Maliakos gulf. Their temperatures range from 32.0°C to 40.6°C and their TDS values range from 9109 ppm to 25041 ppm (high TDS waters). The thermal springs occurring at the northwestern border of the graben are different. They have low TDS waters ranging from 266 ppm to 589 ppm and their temperatures range from 24.3°C to 32.6°C. The genesis and origin of the above thermal mineral waters have been studied on the basis of the hydrogeological conditions of the study area, the hydrochemical analyses of the thermal waters and their isotopic data. |
en |
| heal.journalName |
Neues Jahrbuch fur Geologie und Palaontologie - Monatshefte |
en |
| dc.identifier.issue |
2 |
en |
| dc.identifier.spage |
91 |
en |
| dc.identifier.epage |
115 |
en |