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Scientific paper - Chapter in Book
Geology of the Old Town of Dubrovnik
In: 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 (Ed.). Zagreb: Hrvatsko geološko društvo (HGD), 2023. pp. 131-139. urn:nbn:hr:245:187480
Korbar, Tvrtko; Grgasović, Tonći; Fuček, Ladislav

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Korbar, T., Grgasović, T. & Fuček, L. (2023). Geology of the Old Town of Dubrovnik. In T. Korbar, (Ed.), M. Kovačić, (Ed.), I. Vlahović, (Ed.), 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 (pp. 131-139). Zagreb: Hrvatsko geološko društvo (HGD). Retrieved from 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, edited by Tvrtko Korbar, edited by Marijan Kovačić, edited by Igor Vlahović, Hrvatsko geološko društvo (HGD), 2023, pp. 131-139. https://urn.nsk.hr/urn:nbn:hr:245:187480

Korbar, Tvrtko, Tonći Grgasović and Ladislav Fuček. "Geology of the Old Town of Dubrovnik." In 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, edited by Tvrtko Korbar, edited by Marijan Kovačić, edited by Igor Vlahović, 131-139. Zagreb: Hrvatsko geološko društvo (HGD), 2023. https://urn.nsk.hr/urn:nbn:hr:245:187480

Korbar, T., Grgasović, T. and Fuček, L. (2023) 'Geology of the Old Town of Dubrovnik' in Korbar, T. (ed.), Kovačić, M. (ed.), Vlahović, I. (ed.) 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), pp. 131-139. Available at: https://urn.nsk.hr/urn:nbn:hr:245:187480 (Accessed 19 April 2024)

Korbar T, Grgasović T, Fuček L. Geology of the Old Town of Dubrovnik. In: T. Korbar, ed., M. Kovačić, ed., I. Vlahović, ed. 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. Pp. 131-139. [cited 2024 April 19] Available at: https://urn.nsk.hr/urn:nbn:hr:245:187480

T. Korbar, T. Grgasović and 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 and I. Vlahović, Eds. Zagreb: Hrvatsko geološko društvo (HGD), 2023, pp. 131-139. [Online] Available at: https://urn.nsk.hr/urn:nbn:hr:245:187480

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Metadata
Title (english)Geology of the Old Town of Dubrovnik
AuthorTvrtko Korbar
AuthorTonći Grgasović
AuthorLadislav Fuček
EditorTvrtko Korbar
EditorMarijan Kovačić
EditorIgor Vlahović
Author's institutionCroatian Geological Survey
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Geology and Paleontology
Abstract (english)
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.
Keywords (english)
Languageenglish
Publication typeScientific paper - Chapter in Book
Publication statusPublished
Peer reviewPeer review - international
Publication versionPublished version
Book titleedimentary 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
Numberingpp. 131-139
ISBN978-953-6907-80-9
URN:NBNurn:nbn:hr:245:187480
Publication2023-06-12
Type of resourceText
PublisherHrvatsko geološko društvo (HGD)
Publishing placeZagreb
Access conditionsOpen access
Terms of useLicence In copyright icon
Created on2024-01-24 08:34:21