Pregled bibliografske jedinice broj: 1125241
Adria microplate fragmentation: geophysical perspective
Adria microplate fragmentation: geophysical perspective // Book of Abstracts EGU General Assembly 2021
Beč, Austrija; online, 2021. str. 14133-14133 doi:10.5194/egusphere-egu21-14133 (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 1125241 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Adria microplate fragmentation: geophysical perspective
Autori
Stipčević, Josip ; Belinić Topić, Tena ; Kolínský, Petr ; Herak, Marijan ; Molinari, Irene ; Dasović, Iva
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Book of Abstracts EGU General Assembly 2021
/ - , 2021, 14133-14133
Skup
EGU General Assembly 2021
Mjesto i datum
Beč, Austrija; online, 19.04.2021. - 30.04.2021
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Adria microplate, geophysics, fragmentation
Sažetak
Adriatic microplate (Adria) has been a major component of the central Mediterranean geodynamic history since at least Late Cretaceous time. Although Cenozoic motion of Adria is relatively well established, there remains several open questions regarding its dynamics. This is especially evident when trying to reconstruct the motion of Adria since early Miocene. Although there is a general consensus about the counterclockwise rotation of Adria with respect to Europe, the amount of this rotation is still a matter of vigorous debate. In order to explain various measurements, several models of Adria motion were introduced: 1) Adria moving in conjunction with Africa, 2) Adria moving independently as a single block and 3) Adria moving independently but divided into two fragments. Here we explore the third model by using data from temporary seismic station deployments (AlpArray and AlpArray-CASE) and available permanent stations surrounding the Adriatic Sea. We constructed the tomography image of the Adriatic Sea region using the interstation surface wave dispersion measurements from teleseismic events. Additionally, we test the properties of the Central Adriatic crust by analyzing P-receiver functions from mid-Adriatic island seismic stations. Preliminary results show anomalous lithospheric structure in the Central Adriatic dividing Adria into two sections thus indicating that Adria fragmentation has progressed all the way to the base of the lithosphere.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Geofizika
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Josip Stipčević
(autor)
Marijan Herak
(autor)
Iva Dasović
(autor)
Tena Belinić Topić
(autor)