Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Jens Tómasson"'
Autor:
Pórdur Arason, Jens Tómasson
Publikováno v:
Geothermics. 29:723-735
This study deals with thermal mining in several geothermal systems in Iceland. A number of 2500- to 3000-m deep drillholes have been drilled into low temperature geothermal areas in the country. The conductive gradient outside active geothermal areas
Autor:
Jens Tómasson
Publikováno v:
Geothermics. 22:329-348
The Ellidaar low-temperature system is situated in Quaternary strata in SW-Iceland. It has been utilized for space heating in the city of Reykjavik since 1968. The subsurface rocks may be divided into an upper basalt group, a hyaloclastite group and
Publikováno v:
Mineral and Thermal Groundwater Resources ISBN: 9789401064705
Iceland lies in the North Atlantic Ocean, just south of the Polar Circle. It is formed by the only major subaerial part of the Mid-Atlantic Ridge system (Figure 9.1) and has an area of some 100000km2. The Mid-Atlantic Ridge is represented by the Reyk
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9f88f0be31f764eaf1cfc1447b1936a
https://doi.org/10.1007/978-94-011-5846-6_9
https://doi.org/10.1007/978-94-011-5846-6_9
Autor:
Hrefna Kristmannsdóttir, Jens Tómasson
Publikováno v:
Contributions to Mineralogy and Petrology. 36:123-134
The geothermal area on Reykjanes, Iceland has been investigated mineralogically. The temperature within the studied area is very variable from 30–300° C. Mineral zones corresponding to the temperature conditions in the area are found. Accidental c
Autor:
Jens Tómasson
Publikováno v:
Jökull. 17:300-311
Autor:
Valgardur Stefánsson, Stefán Arnórsson, G. Palmason, Hrefna Kristmannsdóttir, Kristjan Saemundsson, Leo Kristjansson, Ingvar Birgir Fridleifsson, Benedikt Steingrímsson, Jens Tómasson
Publikováno v:
Deep Drilling Results in the Atlantic Ocean: Ocean Crust
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80d1704c87c0b7eaa9a6fbd6a507351b
https://doi.org/10.1029/me002p0043
https://doi.org/10.1029/me002p0043
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