Geothermal studies of the Outokumpu Deep Drill Hole, Finland: Vertical variation in heat flow and palaeoclimatic implications

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F11%3A00365192" target="_blank" >RIV/67985530:_____/11:00365192 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1016/j.pepi.2011.06.002" target="_blank" >http://dx.doi.org/10.1016/j.pepi.2011.06.002</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.pepi.2011.06.002" target="_blank" >10.1016/j.pepi.2011.06.002</a>

Result language
angličtina
Original language name
Geothermal studies of the Outokumpu Deep Drill Hole, Finland: Vertical variation in heat flow and palaeoclimatic implications
Original language description
Detailed geothermal studies of deep drill holes provide insights to heat transfer processes in the crust, and allow separation of different factors involved, such as palaeoclimatic and structural conductive effects as well as advective fluid flow effects. We present high resolution geothermal results of the 2516 m deep Outokumpu Deep Drill Hole in eastern Finland drilled in 2004?2005 into a Palaeoproterozoic formation with metasedimentary rocks, ophiolite-derived altered ultramafic rocks and pegmatiticgranite. The down-hole temperatures have been logged five times after end of drilling and extend to day 948 after drilling.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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