Pregled bibliografske jedinice broj: 211769
Late Neogene Counterclockwise Rotation in the SW Corner of the Pannonian Basin
Late Neogene Counterclockwise Rotation in the SW Corner of the Pannonian Basin // 3. Hrvatski geološki kongres & 7th Workshop on Alpine Geological Studies, Opatija, 29.09.-01.10.2005, ABSTRACTS BOOK / Tomljenović, Bruno ; Balen, Dražen ; Vlahović, Igor ; (ur.).
Zagreb: Hrvatski geološki institut, 2005. str. 55-55 (predavanje, domaća recenzija, sažetak, znanstveni)
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Naslov
Late Neogene Counterclockwise Rotation in the SW Corner of the Pannonian Basin
Autori
Márton, Emoe ; Jelen, Bogomir ; Tomljenović, Bruno ; Pavelić, Davor ; Poljak, Marijan ; Márton, Péter ; Avanić, Radovan ; Pamić, Jakob
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
3. Hrvatski geološki kongres & 7th Workshop on Alpine Geological Studies, Opatija, 29.09.-01.10.2005, ABSTRACTS BOOK
/ Tomljenović, Bruno ; Balen, Dražen ; Vlahović, Igor ; - Zagreb : Hrvatski geološki institut, 2005, 55-55
Skup
3. Hrvatski geološki kongres
Mjesto i datum
Opatija, Hrvatska, 29.09.2005. - 01.10.2005
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Domaća recenzija
Ključne riječi
Paleomagnetism; South Pannonian Basin; Neogene; Rotation
Sažetak
Earlier paleomagnetic studies suggested that counterclockwise rotating Adriatic microplate could have triggered the youngest rotations in the Hrvatsko Zagorje area, in the area of Slavonian Mts. and in the Mura-Zala depression. Since the named areas are located quite far from the Eastern Adriatic coast, we decided to study the Krško and Karlovac basins, which are situated in-between (Fig. 1). From the collected 12 paleomagnetic localities (Badenian through Pontian sediments) ten yielded good paleomagnetic directions as a result of laboratory processing and statistical evaluation. They definitely point to the counterclockwise rotation of the area in post early Pontian times. The angle of the rotation is about 20° (D=337°, I=50°, k=48, 95=10°). Thus, we have found a missing tectonic link from the Hrvatsko Zagorje, Slavonian Mts. and the Mura-Zala basins to the Adriatic microplate and collected further paleomagnetic evidence for the end of Miocene or even younger important tectonic movements in the South Pannonian basin.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Rudarstvo, nafta i geološko inženjerstvo
POVEZANOST RADA
Ustanove:
Hrvatski geološki institut,
Rudarsko-geološko-naftni fakultet, Zagreb