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Pregled bibliografske jedinice broj: 640082

Neotectonics of the Dinarides–Pannonian Basin transition and possible earthquake sources in the Banja Luka epicentral area


Ustaszewski, Kamil; Herak, Marijan; Tomljenović, Bruno; Herak, Davorka; Matej, Srebrenka
Neotectonics of the Dinarides–Pannonian Basin transition and possible earthquake sources in the Banja Luka epicentral area // Journal of geodynamics, 82 (2014), 52-68 doi:10.1016/j.jog.2014.04.006 (međunarodna recenzija, članak, znanstveni)


CROSBI ID: 640082 Za ispravke kontaktirajte CROSBI podršku putem web obrasca

Naslov
Neotectonics of the Dinarides–Pannonian Basin transition and possible earthquake sources in the Banja Luka epicentral area

Autori
Ustaszewski, Kamil ; Herak, Marijan ; Tomljenović, Bruno ; Herak, Davorka ; Matej, Srebrenka

Izvornik
Journal of geodynamics (0264-3707) 82 (2014); 52-68

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
Adriatic plate; Dinarides; Pannonian Basin; fold-and-thrust belt; neotectonics; seismicity; seismotectonics

Sažetak
This study provides evidence for post-5 Ma shortening in the transition area between the Dinarides fold-and-thrust belt and the Pannonian Basin and reviews possible earthquake sources for the Banja Luka epicentral area (northern Bosnia and Herzegovina) where the strongest instrumentally recorded earthquake (ML 6.4) occurred on 27 October 1969. Geological, geomorphological and reflection seismic data provide evidence for a compressive or transpressive reactivation of Late Palaeogene to Middle Miocene normal faults. This reactivation postdates deposition of the youngest sediments in the Pannonian Basin of Pontian age (c. 5 Ma). Fault plane solutions for the main 1969 Banja Luka earthquake (ML 6.4) and its largest foreshock (ML 6.0) indicate reverse faulting along ESE–WNW- striking nodal planes and generally N–S trending pressure axes. The spatial distribution of epicentres and focal depths, analyses of the macroseismic field and fault-plane solutions for several smaller events suggest on-going shortening in the internal Dinarides. Seismic deformation of the upper crust is also associated with strike- slip faults, likely related to the NE–SW trending, sinistral Banja Luka fault, which possibly acts as a transfer fault accommodating residual deformations of adjacent active segments of the Dinarides thrust system. The study area represents the seismically most active region of the Dinarides apart from the Adriatic Sea coast and the bend zone around Zagreb. We propose that on- going thrusting in the internal Dinarides thrust system takes up a portion of the current Adria– Europe convergence.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

Napomena
SI : Geodynamics of the Mediterranean.



POVEZANOST RADA


Projekti:
119-1193086-1314 - Istraživanje geomagnetskog polja i nehomogenosti litosfere u području Hrvatske (Herak, Davorka, MZOS ) ( POIROT)
119-1193086-1315 - Seizmičnost Hrvatske (Herak, Marijan, MZOS ) ( POIROT)
195-1951293-3155 - CROTEC - Strukturna analiza recentne i neotektonske aktivnosti u Hrvatskoj (Tomljenović, Bruno, MZOS ) ( POIROT)

Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Rudarsko-geološko-naftni fakultet, Zagreb

Profili:

Avatar Url Bruno Tomljenović (autor)

Avatar Url Marijan Herak (autor)

Avatar Url Davorka Herak (autor)

Citiraj ovu publikaciju

Ustaszewski, Kamil; Herak, Marijan; Tomljenović, Bruno; Herak, Davorka; Matej, Srebrenka
Neotectonics of the Dinarides–Pannonian Basin transition and possible earthquake sources in the Banja Luka epicentral area // Journal of geodynamics, 82 (2014), 52-68 doi:10.1016/j.jog.2014.04.006 (međunarodna recenzija, članak, znanstveni)
Ustaszewski, K., Herak, M., Tomljenović, B., Herak, D. & Matej, S. (2014) Neotectonics of the Dinarides–Pannonian Basin transition and possible earthquake sources in the Banja Luka epicentral area. Journal of geodynamics, 82, 52-68 doi:10.1016/j.jog.2014.04.006.
@article{article, year = {2014}, pages = {52-68}, DOI = {10.1016/j.jog.2014.04.006}, keywords = {Adriatic plate, Dinarides, Pannonian Basin, fold-and-thrust belt, neotectonics, seismicity, seismotectonics}, journal = {Journal of geodynamics}, doi = {10.1016/j.jog.2014.04.006}, volume = {82}, issn = {0264-3707}, title = {Neotectonics of the Dinarides–Pannonian Basin transition and possible earthquake sources in the Banja Luka epicentral area}, keyword = {Adriatic plate, Dinarides, Pannonian Basin, fold-and-thrust belt, neotectonics, seismicity, seismotectonics} }
@article{article, year = {2014}, pages = {52-68}, DOI = {10.1016/j.jog.2014.04.006}, keywords = {Adriatic plate, Dinarides, Pannonian Basin, fold-and-thrust belt, neotectonics, seismicity, seismotectonics}, journal = {Journal of geodynamics}, doi = {10.1016/j.jog.2014.04.006}, volume = {82}, issn = {0264-3707}, title = {Neotectonics of the Dinarides–Pannonian Basin transition and possible earthquake sources in the Banja Luka epicentral area}, keyword = {Adriatic plate, Dinarides, Pannonian Basin, fold-and-thrust belt, neotectonics, seismicity, seismotectonics} }

Časopis indeksira:


  • Current Contents Connect (CCC)
  • Web of Science Core Collection (WoSCC)
    • Science Citation Index Expanded (SCI-EXP)
    • SCI-EXP, SSCI i/ili A&HCI
  • Scopus


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