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Pregled bibliografske jedinice broj: 1036145

An ensialic volcanic arc along the northwestern edge of Paleotethys – Insights from the Mid-Triassic volcano-sedimentary succession of Ivanščica Mt. (northwestern Croatia)


Slovenec, Damir; Šegvić, Branimir; Halamić, Josip; Goričan, Špela; Zanoni, Giovanni
An ensialic volcanic arc along the northwestern edge of Paleotethys – Insights from the Mid-Triassic volcano-sedimentary succession of Ivanščica Mt. (northwestern Croatia) // Geological journal, 55 (2020), 6; 4324-4351 doi:10.1002/gj.3664 (međunarodna recenzija, članak, znanstveni)


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Naslov
An ensialic volcanic arc along the northwestern edge of Paleotethys – Insights from the Mid-Triassic volcano-sedimentary succession of Ivanščica Mt. (northwestern Croatia)

Autori
Slovenec, Damir ; Šegvić, Branimir ; Halamić, Josip ; Goričan, Špela ; Zanoni, Giovanni

Izvornik
Geological journal (0072-1050) 55 (2020), 6; 4324-4351

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
active continental margin, Croatia, ensialic volcanic arc, Ivanščica Mt., Middle Triassic volcano-sedimentary succession, Palaeotethys, palagonitization

Sažetak
This work aims to unveil the origin, geodynamic significance, and diagenetic history of pyroclastites and associated chert documented within the Upper Anisian volcanosedimentary succession of the Ivanščica Mt. in Central Europe. An abundance of pyroclastic material points to polyphase volcanic activity and deep‐water sedimentation along the rim of an oceanic realm. Radiolarian‐based dating revealed Illyrian age of chert intercalated with pyroclastites. The latter are largely vitro‐crystalloclastic and were emplaced as airborne tuff. The crystalloclasts of sanidine, plagioclase, altered pyroxene, and amphibole are principal tuff constituents merged in the altered glassy matrix consisted of palagonite, clay minerals, and calcite. Variations in alteration assemblages reflect an extensive in situ eogenesis in an open hydrologic system that gradually evolved toward a restricted fluid percolation environment. Mineralogy, chemistry, and occurrence of andesitic tuff clearly denote an explosive volcanic activity formed at the top of suprasubduction zone. Such scenario presumes a complex genesis outlined in following steps: (a) partial melting and dehydration of down‐going Palaeotethyan slab which gave rise to the subduction‐related magmatism {; ; LILE, Th, and LREE [(La/Lu)cn = 6.51−9.42] enrichment ; negative anomalies of Nb‐Ta, P, and Ti [e.g., (Nb/La)n = 0.31−0.44]}; ; ; (b) magma contamination via interaction with continental crust during magma uplift along tectonically weakened zones of upper crust [positive Pb spikes, negative εNd (−4.18 to −4.44), and 147Sm/144Nd ≤ 0.113175]. This is in favour of geodynamic evolution that hypothesizes the existence of an active, ensialic, and mature volcanic arc developed along the southern active continental margins of Euramerica (Laurussia) during Late Anisian subduction of Palaeotethyan lithosphere.

Izvorni jezik
Engleski

Znanstvena područja
Geologija



POVEZANOST RADA


Projekti:
P1-0008
MRI04-511
181-1951126-1141 - Mezozojske magmatske, plaštne i piroklastične stijene sjeverozapadne Hrvatske (Slovenec, Damir, MZOS ) ( POIROT)

Ustanove:
Hrvatski geološki institut

Profili:

Avatar Url Josip Halamić (autor)

Avatar Url Branimir Šegvić (autor)

Avatar Url Damir Slovenec (autor)

Poveznice na cjeloviti tekst rada:

Pristup cjelovitom tekstu rada doi

Citiraj ovu publikaciju:

Slovenec, Damir; Šegvić, Branimir; Halamić, Josip; Goričan, Špela; Zanoni, Giovanni
An ensialic volcanic arc along the northwestern edge of Paleotethys – Insights from the Mid-Triassic volcano-sedimentary succession of Ivanščica Mt. (northwestern Croatia) // Geological journal, 55 (2020), 6; 4324-4351 doi:10.1002/gj.3664 (međunarodna recenzija, članak, znanstveni)
Slovenec, D., Šegvić, B., Halamić, J., Goričan, Š. & Zanoni, G. (2020) An ensialic volcanic arc along the northwestern edge of Paleotethys – Insights from the Mid-Triassic volcano-sedimentary succession of Ivanščica Mt. (northwestern Croatia). Geological journal, 55 (6), 4324-4351 doi:10.1002/gj.3664.
@article{article, year = {2020}, pages = {4324-4351}, DOI = {10.1002/gj.3664}, keywords = {active continental margin, Croatia, ensialic volcanic arc, Ivan\v{s}\v{c}ica Mt., Middle Triassic volcano-sedimentary succession, Palaeotethys, palagonitization}, journal = {Geological journal}, doi = {10.1002/gj.3664}, volume = {55}, number = {6}, issn = {0072-1050}, title = {An ensialic volcanic arc along the northwestern edge of Paleotethys – Insights from the Mid-Triassic volcano-sedimentary succession of Ivan\v{s}\v{c}ica Mt. (northwestern Croatia)}, keyword = {active continental margin, Croatia, ensialic volcanic arc, Ivan\v{s}\v{c}ica Mt., Middle Triassic volcano-sedimentary succession, Palaeotethys, palagonitization} }
@article{article, year = {2020}, pages = {4324-4351}, DOI = {10.1002/gj.3664}, keywords = {active continental margin, Croatia, ensialic volcanic arc, Ivan\v{s}\v{c}ica Mt., Middle Triassic volcano-sedimentary succession, Palaeotethys, palagonitization}, journal = {Geological journal}, doi = {10.1002/gj.3664}, volume = {55}, number = {6}, issn = {0072-1050}, title = {An ensialic volcanic arc along the northwestern edge of Paleotethys – Insights from the Mid-Triassic volcano-sedimentary succession of Ivan\v{s}\v{c}ica Mt. (northwestern Croatia)}, keyword = {active continental margin, Croatia, ensialic volcanic arc, Ivan\v{s}\v{c}ica Mt., Middle Triassic volcano-sedimentary succession, Palaeotethys, palagonitization} }

Časopis indeksira:


  • Current Contents Connect (CCC)
  • Web of Science Core Collection (WoSCC)
    • Science Citation Index Expanded (SCI-EXP)
    • SCI-EXP, SSCI i/ili A&HCI
  • Scopus


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