Počet záznamů: 1
The recognition of transient compressional fault slow-slip along the northern shore of Hornsund Fjord, SW Spitsbergen, Svalbard
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SYSNO ASEP 0447763 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název The recognition of transient compressional fault slow-slip along the northern shore of Hornsund Fjord, SW Spitsbergen, Svalbard Tvůrce(i) Stemberk, Josef (USMH-B) RID, ORCID
Briestenský, Miloš (USMH-B) RID, ORCID
Cacon, S. (PL)Zdroj.dok. Polish Polar Research - ISSN 0138-0338
Roč. 36, č. 2 (2015), s. 109-123Poč.str. 15 s. Forma vydání Tištěná - P Jazyk dok. eng - angličtina Země vyd. PL - Polsko Klíč. slova Arctic ; Svalbard ; Hornsund ; 3-D fault displacement monitoring ; transient slow fault slip Vědní obor RIV DB - Geologie a mineralogie CEP LM2010008 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy Institucionální podpora USMH-B - RVO:67985891 UT WOS 000357358600002 EID SCOPUS 84935083073 DOI 10.1515/popore-2015-0007 Anotace This paper presents the results of direct 3-D fault displacement monitoring along the northern shore of Hornsund Fjord, SW Spitsbergen, Svalbard. The fault displacements have been recorded using three permanently installed optical-mechanical crack gauges since 2009. The monitoring data from all three sites provided evidence for a remarkable slip event that lasted from September 2011 to May 2012. The cause is discussed in some detail with consideration given to both exogenic (temperature changes, surface processes) and endogenic processes (isostatic rebound and regional seismicity). It is proposed that transient fault slips recorded had a tectonic origin and were caused by approximately W-E oriented compression corresponding to regional compression in the Svalbard area. Pracoviště Ústav struktury a mechaniky hornin Kontakt Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216 Rok sběru 2016
Počet záznamů: 1