Fluid geochemistry of Nisyros island, Dodecanese, Greece
Two distinct hydrothermal aquifers are present beneath the Lakki plain: (a) a deep aquifer, characterized by temperatures higher than 290°C and chloride-rich fluids: and (b) a shallow aquifer, with a chloride content close to that of sea water and temperatures in the range 170–255°C. The vapor phase...
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| Veröffentlicht in: | Journal of volcanology and geothermal research 1993-05, Vol.56 (1), p.95-112 |
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| container_title | Journal of volcanology and geothermal research |
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| creator | Chiodini, G. Cioni, R. Leonis, C. Marini, L. Raco, B. |
| description | Two distinct hydrothermal aquifers are present beneath the Lakki plain: (a) a deep aquifer, characterized by temperatures higher than 290°C and chloride-rich fluids: and (b) a shallow aquifer, with a chloride content close to that of sea water and temperatures in the range 170–255°C. The vapor phase boiled from the shallow aquifer feeds the fumarolic vents in the southern half of the Lakki plain and its liquid phase flows northeast and southwest, contributing to the thermal springs located along the northern and southern coasts of the island. This conceptual hydrogeochemical model of Nisyros Island can be used to reconstruct past hydrothermal eruptions and to estimate the risk of such events happening again in the future. |
| doi_str_mv | 10.1016/0377-0273(93)90052-S |
| format | Article |
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The vapor phase boiled from the shallow aquifer feeds the fumarolic vents in the southern half of the Lakki plain and its liquid phase flows northeast and southwest, contributing to the thermal springs located along the northern and southern coasts of the island. This conceptual hydrogeochemical model of Nisyros Island can be used to reconstruct past hydrothermal eruptions and to estimate the risk of such events happening again in the future.</description><identifier>ISSN: 0377-0273</identifier><identifier>EISSN: 1872-6097</identifier><identifier>DOI: 10.1016/0377-0273(93)90052-S</identifier><identifier>CODEN: JVGRDQ</identifier><language>eng</language><publisher>Lausanne: Elsevier B.V</publisher><subject>Crystalline rocks ; Earth sciences ; Earth, ocean, space ; Engineering and environment geology. 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The vapor phase boiled from the shallow aquifer feeds the fumarolic vents in the southern half of the Lakki plain and its liquid phase flows northeast and southwest, contributing to the thermal springs located along the northern and southern coasts of the island. This conceptual hydrogeochemical model of Nisyros Island can be used to reconstruct past hydrothermal eruptions and to estimate the risk of such events happening again in the future.</description><subject>Crystalline rocks</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Geochemistry</subject><subject>Igneous and metamorphic rocks petrology, volcanic processes, magmas</subject><subject>Mineralogy</subject><subject>Natural hazards: prediction, damages, etc</subject><subject>Silicates</subject><subject>Water geochemistry</subject><issn>0377-0273</issn><issn>1872-6097</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1993</creationdate><recordtype>article</recordtype><recordid>eNp9kEFLw0AQhRdRsFb_gYccRBQanc0m2exFkGqrUPRQPS_L7ERX0kR3U6H_3g0tPQoDc_nemzePsXMONxx4eQtCyhQyKa6UuFYARZYuD9iIVzJLS1DykI32yDE7CeELADhUMGLVrFk7m3xQh5-0cqH3m6SrkxcXNr4LiQuNae0keegsoWkp0CSZeyKkU3ZUmybQ2W6P2fvs8W36lC5e58_T-0VqRCX7VKCk3FS1MmWegULiCMaoUlGWKVsgYAkF1tLyQhQkDVcWpUWhTKEii2LMLre-3777WVPodUyJ1MRc1K2D5qXKqlzmEcy3IMbgwVOtv71bGb_RHPRQkx460EMHWsUZatLLKLvY-ZuApqm9adGFvTaXIlNVFbG7LUbx119HXgd01CJZ5wl7bTv3_50_KwF6-g</recordid><startdate>19930501</startdate><enddate>19930501</enddate><creator>Chiodini, G.</creator><creator>Cioni, R.</creator><creator>Leonis, C.</creator><creator>Marini, L.</creator><creator>Raco, B.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope></search><sort><creationdate>19930501</creationdate><title>Fluid geochemistry of Nisyros island, Dodecanese, Greece</title><author>Chiodini, G. ; Cioni, R. ; Leonis, C. ; Marini, L. ; Raco, B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a387t-3c7e4a8f9a64209ce1c0aa969e229d5c0c605cf7d1535e7a19dc7dc39a59e1cc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1993</creationdate><topic>Crystalline rocks</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. 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| ispartof | Journal of volcanology and geothermal research, 1993-05, Vol.56 (1), p.95-112 |
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| language | eng |
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| source | ScienceDirect Journals (5 years ago - present) |
| subjects | Crystalline rocks Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Geochemistry Igneous and metamorphic rocks petrology, volcanic processes, magmas Mineralogy Natural hazards: prediction, damages, etc Silicates Water geochemistry |
| title | Fluid geochemistry of Nisyros island, Dodecanese, Greece |
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