prikaz prve stranice dokumenta Geology of the Old Town of Dubrovnik
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Geology of the Old Town of Dubrovnik
U: edimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin / Korbar, Tvrtko; Kovačić, Marijan; Vlahović, Igor (ur.). Zagreb: Hrvatsko geološko društvo (HGD), 2023. str. 131-139. urn:nbn:hr:245:187480
Korbar, Tvrtko; Grgasović, Tonći; Fuček, Ladislav

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Korbar, T., Grgasović, T. i Fuček, L. (2023). Geology of the Old Town of Dubrovnik. U T. Korbar, (Ur.), M. Kovačić, (Ur.), I. Vlahović, (Ur.), edimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin (str. 131-139). Zagreb: Hrvatsko geološko društvo (HGD). Preuzeto s https://urn.nsk.hr/urn:nbn:hr:245:187480

Korbar, Tvrtko, et al. "Geology of the Old Town of Dubrovnik." edimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin, Ur. Tvrtko Korbar, Ur. Marijan Kovačić, Ur. Igor Vlahović, Hrvatsko geološko društvo (HGD), 2023, str. 131-139. https://urn.nsk.hr/urn:nbn:hr:245:187480

Korbar, Tvrtko, Tonći Grgasović i Ladislav Fuček. "Geology of the Old Town of Dubrovnik." U edimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin, ur. Tvrtko Korbar, ur. Marijan Kovačić, ur. Igor Vlahović, 131-139. Zagreb: Hrvatsko geološko društvo (HGD), 2023. https://urn.nsk.hr/urn:nbn:hr:245:187480

Korbar, T., Grgasović, T. i Fuček, L. (2023) 'Geology of the Old Town of Dubrovnik' u Korbar, T. (ur.), Kovačić, M. (ur.), Vlahović, I. (ur.) edimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin Zagreb: Hrvatsko geološko društvo (HGD), str. 131-139. Preuzeto s: https://urn.nsk.hr/urn:nbn:hr:245:187480 (Datum pristupa: 19.04.2024.)

Korbar T, Grgasović T, Fuček L. Geology of the Old Town of Dubrovnik. U: T. Korbar, ur., M. Kovačić, ur., I. Vlahović, ur. edimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin. Zagreb: Hrvatsko geološko društvo (HGD); 2023. Str. 131-139. [pristupljeno 19.04.2024.] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:245:187480

T. Korbar, T. Grgasović i L. Fuček, "Geology of the Old Town of Dubrovnik", edimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin, T. Korbar, M. Kovačić i I. Vlahović, Ur. Zagreb: Hrvatsko geološko društvo (HGD), 2023, str. 131-139. [Online] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:245:187480

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Podaci o radu
Naslov (engleski)Geology of the Old Town of Dubrovnik
AutorTvrtko Korbar
AutorTonći Grgasović
AutorLadislav Fuček
UrednikTvrtko Korbar
UrednikMarijan Kovačić
UrednikIgor Vlahović
Autorova ustanovaHrvatski geološki institut
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Geologija i paleontologija
Sažetak (engleski)
The Old City of Dubrovnik is on the UNESCO World Heritage list and is recognized as the “Pearl of the Adriatic” that adorns the southern coastal part of the Dinaric Karst. Both the southern and northern elevated parts of the Old Town are built on Mesozoic carbonate rocks deposited on the Adriatic Carbonate Platform (AdCP). The carbonate bedrock is strongly deformed since major compressional deformations of the AdCP succession began in the Eocene during the early orogenic thrusting and formation of the External Dinarides fold and thrust belt. The late orogenic complex tectonic deformations are still ongoing, and the area is characterized by occasional strong seismicity. The deformed packages of stratified limestones and dolomites of the Old Town bedrock show sedimentological features typical of peritidal subtropical sedimentation on the AdCP, while rare key microfossils allow age determination. The northern part of the Old City is situated on the Lower Cretaceous limestones while the southern part is built on the Upper Cretaceous dolomites. The central low-lying part of the town is built on anthropogenic infill of a narrow late Holocene embayment characterized by superficial Quaternary sediments overlying the heavily fractured carbonate bedrock. The exposed karst cavities are mostly filled with speleothems, indicating long-term karstification and denudation. The southern rocky shore is in patches covered by thin recent supratidal aragonitic encrustations known as pelagosite. Since geodetic data and coastal geomorphological features indicate recent surface deformations, the newly discovered geological structure of the Old Town of Dubrovnik should be taken into consideration during regional seismo-tectonic investigations.
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Poglavlje u knjizi
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov knjigeedimentary cover of the Adria and its surroundings: from aborted rifting in the central Adriatic to the post-collisional deposition in the Dinarides, the Southern Alps, and the Pannonian basin
Brojčani podacistr. 131-139
ISBN978-953-6907-80-9
URN:NBNurn:nbn:hr:245:187480
Datum objave publikacije2023-06-12
Vrsta resursaTekst
IzdavačHrvatsko geološko društvo (HGD)
Mjesto izdavanjaZagreb
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Zaštićeno autorskim pravom.
Datum i vrijeme pohrane2024-01-24 08:34:21