Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling

Šumanovac, Franjo

doi:10.3390/geosciences12120439

prikaz prve stranice dokumenta Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling

Znanstveni rad - Izvorni znanstveni rad

Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling

Geosciences, 12 (2022), 12; 439. https://doi.org/10.3390/geosciences12120439

Šumanovac, Franjo

Citirajte ovaj rad

APA 6th Edition

Šumanovac, F. (2022). Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling. Geosciences, 12. (12). doi: 10.3390/geosciences12120439

MLA 8th Edition

Šumanovac, Franjo. "Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling." Geosciences, vol. 12, br. 12, 2022. https://doi.org/10.3390/geosciences12120439

Chicago 17th Edition

Šumanovac, Franjo. "Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling." Geosciences 12, br. 12 (2022). https://doi.org/10.3390/geosciences12120439

Harvard

Šumanovac, F. (2022) 'Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling', Geosciences, 12(12). doi: 10.3390/geosciences12120439

Vancouver

Šumanovac F. Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling. Geosciences [Internet]. 29.11.2022. [pristupljeno 08.05.2024.];12(12). doi: 10.3390/geosciences12120439

IEEE

F. Šumanovac, "Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling", Geosciences, vol. 12, br. 12, Studeni 2022. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:666771. [Citirano: 08.05.2024.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:169:666771

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Naslov (engleski)	Lithosphere structure of the Southern Dinarides and continuity of the Adriatic lithosphere slab beneath the Northern Dinarides unravelled by seismic modelling
Autor	Franjo Šumanovac
Autorova ustanova	Sveučilište u Zagrebu Rudarsko-geološko-naftni fakultet (Zavod za geofizička istraživanja i rudarska mjerenja)
Znanstveno / umjetničko područje, polje i grana	PRIRODNE ZNANOSTI Geologija
Znanstveno / umjetničko područje, polje i grana	PRIRODNE ZNANOSTI Geofizika
Znanstveno / umjetničko područje, polje i grana	TEHNIČKE ZNANOSTI Rudarstvo, nafta i geološko inženjerstvo
Sažetak (engleski)	Currently recognised lithospheric models hypothesise the non-existence of a lithospheric slab (a so-called slab gap) in the area of the Northern Dinarides, and the possible existence of a shallow slab in the Southern Dinarides. These geological models are mostly based on previous regional and global 3D velocity models obtained from teleseismic tomography. Recent local tomographic models providing a good resolution have regularly shown the existence of a fast anomaly underneath the entire Dinarides, directly indicating the existence of a lithospheric slab. To avoid interpretation pitfalls and increase reliability, forward seismic modelling based on new tomographic models was performed. Seismic modelling indicates a continuous lithospheric slab along the entire Dinarides in the shallow mantle, but it is not continuous vertically. In the Northern Dinarides, the shallow lithospheric slab extends at least to a depth of 150 km. In the Southern and Central Dinarides, there is a deep fast anomaly that can be interpreted in two ways due to the weak vertical resolution of teleseismic tomography. The first model suggests a steeply dipping continuous Adriatic lithospheric slab whereas the second model shows that the slab consists of two separate blocks, meaning that the deeper block was formed by delamination of the Adriatic lithospheric slab. Due to a similar correlation between the inverse velocity models for the synthetic model and the observed data, preference is not given to any model. The second model could indicate two independent Dinaridic subduction phases, as opposed to viewing subduction as a single long process during the geological past.
Ključne riječi (engleski)
Jezik	engleski
Vrsta publikacije	Znanstveni rad - Izvorni znanstveni rad
Status objave	Objavljen
Vrsta recenzije	Recenziran - međunarodna recenzija
Verzija publikacije	Objavljena verzija rada (izdavačev PDF)
Naslov časopisa	Geosciences
Brojčani podaci	vol. 12, br. 12, 439
e-ISSN	2076-3263
DOI	https://doi.org/10.3390/geosciences12120439
URN:NBN	urn:nbn:hr:169:666771
Datum objave publikacije	2022-11-29
Projekt	Šifra: KK.01.1.1.02.0022 Naziv (hrvatski): Virtulab – Integrirani laboratorij za primarne i sekundarne sirovine Kratica: Virtulab Voditelj: Sibila Borojević Šoštarić Pravna nadležnost: Hrvatska Financijer: EK Linija financiranja: EFRR
URL dokumenta	https://www.mdpi.com/2076-3263/12/12/439
Vrsta resursa	Tekst
Prava pristupa	Otvoreni pristup
Uvjeti korištenja
Datum i vrijeme pohrane	2024-02-01 09:36:03