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Synthrusting remagnetization of the Krížna nappe: high resolution palaeo- and rock magnetic study in the Strážovce section, Strážovské vrchy Mts, Central West Carpathians (Slovakia)
Title Synthrusting remagnetization of the Krížna nappe: high resolution palaeo- and rock magnetic study in the Strážovce section, Strážovské vrchy Mts, Central West Carpathians (Slovakia) Author Grabowski Jacek Co-authors Michalík Jozef 1946 - SAVGEOL ; SAVUVOZ - Geologický ústav SAV SCOPUS ORCID Szaniawski Rafał Grotek Izabella Source document Acta Geologica Polonica. Vol. 59, no. 2 (2009), p. 137-155 Language eng - English Country PL - Poland Document kind rozpis článkov z periodík (rbx) Citations OLIVA-URCIA, B. - CASAS, A. M. - PUEYO, E. L. at al. Paleomagnetic evidence for dextral strike-slip motion in the Pyrenees during alpine convergence (Mauleon basin, France). In Tectonophysics, 2010, vol. 494, no. 3-4, p. 165-179. DEVLEESCHOUWER, X. - PETITCLERC, E. - SPASSOV, S. et al. The Givetian-Frasnian boundary at names parastratotype (Belgium): the magnetic susceptibility signal controlled by ferromagnetic minerals. In Geologica Belgica, 2010, vol. 13, no. 4, p. 351-366. ZABIELSKI, R. - IWANOV, A. New tectonic elements in the Krížna nappe between Bystra Valley and Strążyska Valley in the Tatra Mts. In Przeglad Geologiczny, 2014, Vol. 62, N. 2, p. 86-96. SATOLLI, Sara - TURTU, Antonio - DONATELLI, Ugo. Magnetostratigraphy of the Salto del Cieco section (Northern Apennines, Italy) from the Pliensbachian to Jurassic/Cretaceous boundary. In NEWSLETTERS ON STRATIGRAPHY. ISSN 0078-0421, 2015, vol. 48, no. 2, pp. 153. Category ADCA - Scientific papers in foreign journals registered in Current Contents Connect with IF (impacted) Category of document (from 2022) V3 - Vedecký výstup publikačnej činnosti z časopisu Type of document článok Year 2009 Registered in WOS Registered in SCOPUS Registered in CCC 
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rok CC IF IF Q (best) JCR Av Jour IF Perc SJR SJR Q (best) CiteScore A rok vydania rok metriky IF IF Q (best) SJR SJR Q (best) 2009 2008 0.581 Q3 0.577 Q2
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