Naslov
THE ALPARRAY-CASE SEISMIC EXPERIMENT: INVESTIGATION OF THE CENTRAL ADRIATIC LITHOSPHERE STRUCTURE

Autori
Dasović, Iva ; Molinari, Irene ; Stipčević, Josip ; Šipka, Vesna ; Kissling, m Edi ; Clinton, John ; Salimbeni, Simone ; Prevolnik, Snježan ; Giardini, Domenico ; Wiemer, Stefan ; AlpArray-CASE Field Team (6), AlpArray-CASE Working Group

Kolaboracija
AlpArray-CASE Field Team ; AlpArray-CASE Working Group

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Book of Abstracts of the 36th General Assembly of the European Seismological Commission / D'Amico, Sebastiano ; Galea, Pauline ; Bozionelos, George ; Colica, Emanuele ; Farrugia, Daniela ; Agius, Matthew - Valletta : University of Malta, 2018, ESC2018-S3-769-ESC2018-S3-769

ISBN
978-88-98161-12-6

Skup
36th General Assembly of the European Seismological Commission

Mjesto i datum
Valletta, Malta, 02.09.2018. - 07.09.2018

Vrsta sudjelovanja
Poster

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Adriatic microplate ; Central Adriatic Seismic Experiment (CASE) ; theoretical ray coverage ; ambient noise tomography

Sažetak
The Adriatic microplate forms the upper plate in the collision front in the Western and Central Alps whereas it forms the lower plate in contact with the Apennines and the Dinarides. However, the tectonics of Adriatic microplate is yet not well constrained and remains controversial, especially at its contact with the Dinarides. While the northern part of the Adriatic microplate will be accurately imaged within the AlpArray project, its central and southern parts deserve detailed studies to obtain a complete picture of its structure and evolution. We set up the Central Adriatic Seismic Experiment (CASE) as an AlpArray Complementary Experiment with a temporary seismic network to provide high-quality seismological data as a foundation for research with state-of-the-art methods and high-precision seismic images of the controversial area. The international AlpArray-CASE project involves four institutions: the Department of Earth Sciences and the Swiss Seismological Service of ETH Zürich (CH), the Department of Geophysics of the Faculty of Science at the University of Zagreb (HR), the Republic Hydrometeorological Service of the Republic of Srpska (BIH) and Istituto Nazionale di Geofisica e Vulcanologia (I). The established temporary seismic network will be operational for at least 18 months. It combines existing permanent and temporary seismic stations operated by the involved institutions together with newly deployed temporary seismic stations, installed in November and December 2016, managed by ETH Zürich and INGV: five in Croatia, four in Bosnia and Herzegovina and one in Italy. We present our scientific aims and network geometry as well as newly deployed stations sites and settings. In particular, the new stations show favourable noise level (power spectral density estimates). The new network improves considerably the theoretical ray coverage for ambient noise tomography and the magnitude threshold shown in the Bayesian magnitude of completeness threshold map.

Izvorni jezik
Engleski

Znanstvena područja
Geofizika

POVEZANOST RADA