Počet záznamů: 1
Geothermal studies of the Outokumpu Deep Drill Hole, Finland: Vertical variation in heat flow and palaeoclimatic implications
- 1.
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, RIDZdroj.dok. Physics of the Earth and Planetary Interiors. - : Elsevier - ISSN 0031-9201
Roč. 188, č. 1-2 (2011), s. 9-25Poč.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