Pregled bibliografske jedinice broj: 1218990
Some indicators of seismic activity in the caves of the Dinaric Karst of Croatia
Some indicators of seismic activity in the caves of the Dinaric Karst of Croatia // Proceeging of the 18th International Congress of Speleology. Karstologia- Memoires 24, , Volume IV. Geomorphology / Gauchon, Christophe ; Jaillet, Stephane (ur.).
Pariz: Federacion Francaise de Speleologie ; International Union of Speleology, 2022. str. 49-52 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
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Naslov
Some indicators of seismic activity in the caves of
the Dinaric Karst of Croatia
Autori
Garašić, Davor ; Garašić, Mladen
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Proceeging of the 18th International Congress of Speleology. Karstologia- Memoires 24, , Volume IV. Geomorphology
/ Gauchon, Christophe ; Jaillet, Stephane - Pariz : Federacion Francaise de Speleologie ; International Union of Speleology, 2022, 49-52
ISBN
9782741706946
Skup
18th International Congress of Speleology
Mjesto i datum
Le Bourget-du-Lac, Francuska, 24.07.2022. - 31.07.2022
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Speleology, Caves, seismic activity, Croatia
Sažetak
The Dinaric karst is located in a seismically very active area. It is the area of contact between the African geotectonic plate and the Eurasian tectonic plate. The Adriatic plate is the northernmost part of the African plate. In the area of the Adriatic Sea, it subducts under the Dinarides. With such displacement of large tectonic plates, strong earthquakes are a common occurrence. Traces of seismotectonics were discovered in some caves. These traces indicate the possible intensity of the earthquakes from the time when seismology did not exist. Recent measurements of the absolute displacements of parts of the speleothem or even parts of cave channels within the last fifty years may have provided additional information on seismic activity. Special attention was paid to the construction of tunnels, bridges, dams and roads when traces of neotectonic movements were noticed inside the discovered caverns. Examples of the effects of recent earthquakesin some cavernsfound in tunnels during construction are given. Changes in the movement and amount of groundwater in these places were detected. Such observations significantly help in creating a more realistic interpretation of speleogenesis in certain karst areas within the Dinarides.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Rudarstvo, nafta i geološko inženjerstvo
POVEZANOST RADA
Ustanove:
Građevinski fakultet, Zagreb,
Hrvatska akademija znanosti i umjetnosti
