prikaz prve stranice dokumenta Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia)
  Preuzmi
PDF 9.86 MB
Znanstveni rad - Izvorni znanstveni rad
Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia)
Geologica Carpathica, 73 (2022), 3; 207-229. https://doi.org/10.31577/GeolCarp.73.3.3
Belak, Mirko; Slovenec, Damir; Kolar-Jurkovšek, Tea; Garašić, Vesnica; Pécskay, Zoltan; Tibljaš, Darko; Mišur, Ivan

Citirajte ovaj rad

Belak, M., Slovenec, D., Kolar Jurkovšek, T., Garašić, V., Pécskay, Z., Tibljaš, D. i Mišur, I. (2022). Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia). Geologica Carpathica, 73. (3), 207-229. doi: 10.31577/GeolCarp.73.3.3

Belak, Mirko, et al. "Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia)." Geologica Carpathica, vol. 73, br. 3, 2022, str. 207-229. https://doi.org/10.31577/GeolCarp.73.3.3

Belak, Mirko, Damir Slovenec, Tea Kolar Jurkovšek, Vesnica Garašić, Zoltan Pécskay, Darko Tibljaš i Ivan Mišur. "Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia)." Geologica Carpathica 73, br. 3 (2022): 207-229. https://doi.org/10.31577/GeolCarp.73.3.3

Belak, M., et al. (2022) 'Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia)', Geologica Carpathica, 73(3), str. 207-229. doi: 10.31577/GeolCarp.73.3.3

Belak M, Slovenec D, Kolar Jurkovšek T, Garašić V, Pécskay Z, Tibljaš D, i sur.. Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia). Geologica Carpathica [Internet]. 26.06.2022. [pristupljeno 13.11.2024.];73(3):207-229. doi: 10.31577/GeolCarp.73.3.3

M. Belak, et al., "Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia)", Geologica Carpathica, vol. 73, br. 3, str. 207-229, Lipanj 2022. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:399722. [Citirano: 13.11.2024.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:169:399722
Prijavite se u repozitorij kako biste mogli spremiti objekt u svoju listu.
Podaci o radu
Naslov (engleski)Low-grade metamorphic rocks of the Tethys subduction–collision zone in the Medvednica Mt. (NW Croatia)
AutorMirko Belak
AutorDamir Slovenec
AutorTea Kolar-Jurkovšek
AutorVesnica Garašić
AutorZoltan Pécskay
AutorDarko Tibljaš
AutorIvan Mišur
Autorova ustanovaHrvatski geološki institut
Autorova ustanovaSveučilište u Zagrebu
Prirodoslovno-matematički fakultet
(Geološki odsjek)
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za mineralogiju, petrologiju i mineralne sirovine)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Sažetak (engleski)
The low-grade metasedimentary rocks of Medvednica Mt. (Northwest Croatia) are associated with orthogreenschists (metabasalts). The Lower to Upper Triassic age of the protolith of the low-grade metamorphic rocks belonging to the Stari Potok, Adolfovac, Tusti Breg, Bliznec, Mrzljak, and Sljeme lithostratigraphic units is determined on the basis of conodonts and field relationships. The metamorphic age of the Triassic metasedimentary rocks from the Risnjak lithostratigraphic units is assumed to be Jurassic. Petrographic and geochemical analyses of ortho-greenschists point to a tholeiite basic magmatic protolith rock having T-MORB (transitional midocean-ridge basalt) characteristics. The ortho-greenschists of the Sljeme lithostratigraphic unit underwent retrograde metamorphism and show metamorphic zoning from the epidote–amphibolite facies to the lower parts of the greenschist facies. However, the greenschists of the Tusti Breg and Bliznec units are characterized by prograde metamorphism ranging from lower to higher greenschist facies. This metamorphism is associated with Jurassic subduction (165–150 Ma) and closure of the Western Tethys. Retrograde metamorphism took place during the collision of the Adriatic and Eurasian plates in the Lower Cretaceous (125–110 Ma).
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaGeologica Carpathica
Brojčani podacivol. 73, br. 3, str. 207-229
p-ISSN1335-0552
e-ISSN1336-8052
DOIhttps://doi.org/10.31577/GeolCarp.73.3.3
URN:NBNurn:nbn:hr:169:399722
Datum objave publikacije2022-06-26
ProjektŠifra: IP-2019-04-3824
Naziv (hrvatski): Vulkano-sedimentne sukcesije sjeverozapadne Hrvatske i njihova uloga u razumijevanju geodinamike Paleotetisa tijekom srednjeg trijasa
Naziv (engleski): Revealing the Middle Triassic Paleotethyan geodynamics recorded in the volcano-sedimentary successions of NW Croatia
Kratica: GOST
Voditelj: Damir Slovenec
Pravna nadležnost: Hrvatska
Financijer: HRZZ
Linija financiranja: IP
ProjektŠifra: 181-1811096-1093
Naziv (hrvatski): Osnovna geološka karta Republike Hrvatske 1:50.000
Naziv (engleski): Basic Geological Map of the Republic of Croatia 1:50.000
Voditelj: Mirko Belak
Pravna nadležnost: Hrvatska
Financijer: MZOS
Linija financiranja: ZP
URL dokumentahttp://www.geologicacarpathica.com/browse-journal/volumes/73-3/article-1008/
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje-Nekomercijalno-Bez prerada 4.0 međunarodna (CC BY-NC-ND 4.0)
Datum i vrijeme pohrane2023-02-01 10:55:00