Geothermal studies of the Outokumpu Deep Drill Hole
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F11%3A00368258" target="_blank" >RIV/67985530:_____/11:00368258 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Geothermal studies of the Outokumpu Deep Drill Hole
Original language description
We present high resolution geothermal results from 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. Detailed geothermal studies of deep drill holes provide insights into heat transfer processes in the crust, and allow the separation of different factors involved, such as palaeoclimatic and structural conductive effects as well as advective fluid flow effects. The down-hole temperatures of the Outokumpu hole have been logged five times following the end of drilling and extend to day 948 after drilling.
Czech name
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Czech description
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Classification
Type
C - Chapter in a specialist book
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Book/collection name
Outokumpu Deep Drilling Project 2003-2010
ISBN
978-952-217-151-1
Number of pages of the result
18
Pages from-to
181-198
Number of pages of the book
252
Publisher name
Geological Survey of Finland
Place of publication
Espoo
UT code for WoS chapter
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