Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Nevena Andrić-Tomašević"'
Autor:
Sierd Cloetingh, Alexander Koptev, István Kovács, Taras Gerya, Anouk Beniest, Ernst Willingshofer, Todd A. Ehlers, Nevena Andrić‐Tomašević, Svetlana Botsyun, Paul R. Eizenhöfer, Thomas François, Fred Beekman
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 2, Pp n/a-n/a (2021)
Abstract Although many different mechanisms for subduction initiation have been proposed, only few of them are viable in terms of consistency with observations and reproducibility in numerical experiments. In particular, it has recently been demonstr
Externí odkaz:
https://doaj.org/article/0580c68e7c3c45169e8e0cbc7dd2a182
Autor:
Vladimir Simić, Zoran Miladinović, Kristina Šarić, Nevena Andrić-Tomašević, Nikola Vuković, Rajko Kondžulović
Publikováno v:
Acta Montanistica Slovaca
Antina Čuka listvenite originated by hydrothermal alteration of small ophiolite mass caused by Paleogene magmatic activity. Mineralogical and petrological examination of the listvenite revealed serpentine-rich, silica-rich, and carbonate-rich variet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6497e80ec1a4b068121e9b804d60fc1b
https://doi.org/10.46544/ams.v27i4.14
https://doi.org/10.46544/ams.v27i4.14
Slab break-off is usually referred to as an early collisional process driven primarily by the slowing of the subduction rate as negatively buoyant oceanic lithosphere detaches from positively buoyant continental lithosphere that is attempting to subd
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a54dd20c81c7937ce8a4798f91bcd7ad
https://doi.org/10.5194/egusphere-egu23-1559
https://doi.org/10.5194/egusphere-egu23-1559
Autor:
Giridas Maiti, Attila Balázs, Lucas Eskens, Taras Gerya, Alexander Koptev, Nevena Andrić-Tomašević
Foreland basins develop in front of growing mountain belts due to the flexure of the downgoing plate in response to forces from slab pull and a topographic load. Many foreland basins worldwide show along-strike variable basin subsidence and architect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4711bdafcef85363c3acd880f3d7f061
https://doi.org/10.5194/egusphere-egu23-812
https://doi.org/10.5194/egusphere-egu23-812
The Central Paratethys Sea occupied the transition between the Alps, Dinarides and Carpathian mountains during Oligocene to Miocene times. However, its spatial and temporal evolution, i.e. southward expansion, subsequent salinity crisis, and governin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dfc667e7624e9975db64490b47b2ccec
https://doi.org/10.5194/egusphere-egu23-9107
https://doi.org/10.5194/egusphere-egu23-9107
Autor:
Lucas H.J. Eskens, Nevena Andrić-Tomašević, Todd A. Ehlers, Peter M. Süss, Matthias Müller, Rolf Herrmann
The Northern Alpine Foreland Basin, also known as the Molasse Basin, developed as a flexural response to the loading of the European plate by the Alpine thrust wedge during a continental collision between the Adriatic and European plates. Along-strik
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2a235b017cd632d37d88ce346ee9d43
Publikováno v:
Earth and Planetary Science Letters, 610, Art.-Nr.: 118097
Earth and Planetary Science Letters
Earth and Planetary Science Letters
The propagation of slab break-off (slab tearing) is usually attributed to laterally variable plate convergence systems with a spatial transition between simultaneous oceanic subduction and continental collision. To study the process of slab tearing i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b66f90169f8da43f130dc4e6801e226
https://doi.org/10.1016/j.epsl.2023.118097
https://doi.org/10.1016/j.epsl.2023.118097
Autor:
Lucas Eskens, Nevena Andrić-Tomašević, Peter M. Süss, Todd A. Ehlers, Rolf Herrmann, Matthias Müller
The Northern Alpine Foreland Basin developed in response to the collision between the European and Adriatic plates. During the Oligocene-Early Miocene coeval along-strike deposition of terrestrial and deep marine conditions are recorded in the wester
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a17980813a47f86187a7c23bd9843fc
https://doi.org/10.5194/egusphere-egu22-4500
https://doi.org/10.5194/egusphere-egu22-4500
Publikováno v:
18. Kongres geologa Srbije "Geologija rešava probleme", Divčibare, 01-04 jun 2022.
187 М60 М64 Donjemiocenski ugljonosni Ibarski basen se nalazi u južnoj Srbiji. Intramontanski ektenzivni basen, izdužen u pravcu severozapad-jugoistok ispunjen je slatkovodnim sedimentima koji su formirani kao deo Dinarskog neogenog jezerskog sis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_____10287::f9fbf9de8322b6f66c992aed4ac2928a
http://dr.rgf.bg.ac.rs/s/repo/item/6970
http://dr.rgf.bg.ac.rs/s/repo/item/6970
Autor:
Viktoria Georgieva, Christoph Glotzbach, Todd A. Ehlers, Sarah Falkowski, Nevena Andrić-Tomašević, Manfred R. Strecker
Publikováno v:
Journal of Geophysical Research: Earth Surface. 126
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ad8eea3eb3e4c04ece1f5e8c2798451
https://doi.org/10.1029/2020jf005993
https://doi.org/10.1029/2020jf005993