Počet záznamů: 1

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

SYSNO ASEP	0365192
Druh ASEP	J - Článek v odborném periodiku
Zařazení RIV	J - Článek v odborném periodiku
Poddruh J	Článek ve WOS
Název	Geothermal studies of the Outokumpu Deep Drill Hole, Finland: Vertical variation in heat flow and palaeoclimatic implications
Tvůrce(i)	Kukkonen, I. T. (FI) Rath, V. (ES) Kivekäs, L. (FI) Šafanda, Jan (GFU-E)_{ORCID, RID} Čermák, Vladimír (GFU-E)_{ORCID, RID}
Zdroj.dok.	Physics of the Earth and Planetary Interiors. - : Elsevier - ISSN 0031-9201 Roč. 188, č. 1-2 (2011), s. 9-25
Poč.str.	17 s.
Jazyk dok.	eng - angličtina
Země vyd.	NL - Nizozemsko
Klíč. slova	heat flow ; geothermal gradient ; thermal conductivity ; paleoclimatology ; Fennoscandian Shield
Vědní obor RIV	DC - Seismologie, vulkanologie a struktura Země
CEZ	AV0Z30120515 - GFU-E (2005-2011)
UT WOS	000297086400002
DOI	10.1016/j.pepi.2011.06.002
Anotace	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 pegmatitic granite. The down-hole temperatures have been logged five times after end of drilling and extend to day 948 after drilling.
Pracoviště	Geofyzikální ústav
Kontakt	Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
Rok sběru	2012

Počet záznamů: 1