prikaz prve stranice dokumenta Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces
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Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces
Scientific Reports, 11 (2021); 2685. https://doi.org/10.1038/s41598-021-81561-5
Balling, Philipp; Grützner, Christoph; Tomljenović, Bruno; Spakman, Wim; Ustaszewski, Kamil

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Balling, P., Grützner, C., Tomljenović, B., Spakman, W. i Ustaszewski, K. (2021). Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces. Scientific Reports, 11.. doi: 10.1038/s41598-021-81561-5

Balling, Philipp, et al. "Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces." Scientific Reports, vol. 11, 2021. https://doi.org/10.1038/s41598-021-81561-5

Balling, Philipp, Christoph Grützner, Bruno Tomljenović, Wim Spakman i Kamil Ustaszewski. "Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces." Scientific Reports 11 (2021). https://doi.org/10.1038/s41598-021-81561-5

Balling, P., et al. (2021) 'Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces', Scientific Reports, 11. doi: 10.1038/s41598-021-81561-5

Balling P, Grützner C, Tomljenović B, Spakman W, Ustaszewski K. Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces. Scientific Reports [Internet]. 29.01.2021. [pristupljeno 04.11.2024.];11. doi: 10.1038/s41598-021-81561-5

P. Balling, C. Grützner, B. Tomljenović, W. Spakman i K. Ustaszewski, "Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces", Scientific Reports, vol. 11, Siječanj 2021. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:592591. [Citirano: 04.11.2024.]

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Naslov (engleski)Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces
AutorPhilipp Balling
AutorChristoph Grützner https://orcid.org/0000-0003-0777-2751
AutorBruno Tomljenović
AutorWim Spakman https://orcid.org/0000-0002-9557-778X
AutorKamil Ustaszewski https://orcid.org/0000-0002-1642-5842
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za geologiju i geološko inženjerstvo)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Sažetak (engleski)
Abstract The Dinarides fold-thrust belt on the Balkan Peninsula resulted from convergence between the Adriatic and Eurasian plates since Mid-Jurassic times. Under the Dinarides, S-wave receiver functions, P-wave tomographic models, and shear-wave splitting data show anomalously thin lithosphere overlying a short down-flexed slab geometry. This geometry suggests a delamination of Adriatic lithosphere. Here, we link the evolution of this continental convergence system to hitherto unreported sets of extensively uplifted Oligocene–Miocene (28–17 Ma) marine terraces preserved at elevations of up to 600 m along the Dinaric coastal range. River incision on either side of the Mediterranean-Black Sea drainage divide is comparable to the amounts of terrace uplift. The preservation of the uplifted terraces implies that the most External Dinarides did not experience substantial deformation other than surface uplift in the Neogene. These observations and the contemporaneous emplacement of igneous rocks (33–22 Ma) in the internal Dinarides suggest that the Oligo-Miocene orogen-wide uplift was driven by post-break-off delamination of the Adriatic lithospheric mantle, this was followed by isostatic readjustment of the remaining crust. Our study details how lithospheric delamination exerts an important control on crustal deformation and that its crustal signature and geomorphic imprint can be preserved for millions of years.
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaScientific Reports
Brojčani podacivol. 11, 2685
e-ISSN2045-2322
DOIhttps://doi.org/10.1038/s41598-021-81561-5
URN:NBNurn:nbn:hr:169:592591
Datum objave publikacije2021-01-29
URL dokumentahttp://www.nature.com/articles/s41598-021-81561-5
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje 4.0 međunarodna (CC BY 4.0)
Datum i vrijeme pohrane2021-02-09 11:12:06