Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Ladislav Fuček"'
Autor:
Tvrtko Korbar, Snježana Markušić, Ozren Hasan, Ladislav Fuček, Dea Brunović, Nikola Belić, Damir Palenik, Vanja Kastelic
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Active tectonics in long-lived orogenic belts usually manifests on the preexisting inherited structures. In the Kvarner region of the External Dinarides, an area with low-to-moderate seismicity related to the Adriatic microplate (Adria) northward mov
Externí odkaz:
https://doaj.org/article/18d60efd5317463fb4bc0863d73c2f5e
Stratigraphy and Tectonic Relationships Along the Senj - Ogulin Profile (Velika Kapela Mt., Croatia)
Publikováno v:
Geologia Croatica, Vol 50, Iss 2, Pp 261-268 (2010)
Twelve lithostratigraphic units, representing a 5 km thick succession,have been determined from the Senj -Ogulin profile through theVelika Kapela Mt. This 45 km long sequence lies approximately normalto the Dinaric strike. Carbonate deposits ranging
Externí odkaz:
https://doaj.org/article/13960b6d6bc7430eb22103696d8f98d4
Autor:
Igor Vlahović, Josip Tišljar, Ladislav Fuček, Nenad Oštrić, Božo Prtoljan, Ivo Velić, Dubravko Matičec
Publikováno v:
Geologia Croatica, Vol 55, Iss 1, Pp 45-55 (2002)
On the NE slopes of Ćićarija Mt. (N Istria) a 120-150 m thick complexcomposed of dolomite-limestone breccia crops out between theLower and Upper Cretaceous deposits. This studied breccia sequenceis of post-sedimentary, tectogenic-diagenetic origin.
Externí odkaz:
https://doaj.org/article/eb3d764afe3c4ac5ba189b4ec9f09ae0
Ivanščica Mt. is an inselberg in the transitional area where S-verging Southern Alpine structures overprint NNW-verging Dinaric structures (van Gelder et al. 2015, and references therein). It is composed of Triassic to Cretaceous shallow to deep-ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4af6842d52e4674098e663210455de3
https://doi.org/10.5194/egusphere-alpshop2022-23
https://doi.org/10.5194/egusphere-alpshop2022-23
Publikováno v:
Geologia Croatica
Volume 73
Issue 2
Volume 73
Issue 2
Maastrichtian to Palaeocene pelagic carbonates on the central Adriatic island of Svetac (Sveti Andrija) are the only outcrops reported to date that document pelagic deposition during the Cretaceous–Palaeogene (K–Pg) transition within the Adriatic
Publikováno v:
Geologia Croatica
Volume 72
Issue 3
Volume 72
Issue 3
The area of the Vinodol Valley and Bakar Bay represents a NW‒SE oriented valley in the NW Adriatic characterised by prominent historical and instrumentally recorded seismicity. As part of the greater geodynamic domain including the Ilirska Bistrica
Publikováno v:
Cretaceous Research
Volume 125
Volume 125
The Cenomanian–Turonian boundary (CTB) on the intra-Tethyan Adriatic Carbonate Platform (AdCP) is generally characterised by a transition between microbially laminated and/or bioclastic limestones to calcisphere-rich massive limestone with bioturba
Publikováno v:
Terra Nova. 29:332-334
We disagree with many of the concerns raised by Font et al., (2017) and take this opportunity to clarify matters. We wish to emphasise that in our paper (Korbar et al., 2017), as well as in the first report on the “potential” Cretaceous–Palaeog
We show crucial evidence for the Cretaceous–Palaeogene (K–Pg) boundary event recorded within a rare succession deposited in an inner-platform lagoon on top of a Mesozoic, tropical, intra-oceanic (western Tethys) Adriatic carbonate platform, which
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4602ce0b31c5ed702b2a34f5f1658e8b
https://orca.cardiff.ac.uk/id/eprint/98381/1/2017_Korbar_et_al_TerraNova_ACCEPTED.pdf
https://orca.cardiff.ac.uk/id/eprint/98381/1/2017_Korbar_et_al_TerraNova_ACCEPTED.pdf
Autor:
Marija Horvat, Ladislav Fuček, Ivan Mišur, Anita Grizelj, Bosiljka Glumac, Hrvoje Posilović, Vlatko Brčić
The Cenomanian–Turonian boundary (CTB) in the Cicarija Mountain region (northern Istria, Croatia) is characterized by calcisphere limestone successions with a firmground and glauconite horizon, bioturbated intervals, tempestites, and slumped struct
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a16d9c897fed6d3137ceabdb930adb63
https://www.bib.irb.hr/871146
https://www.bib.irb.hr/871146