Collected Item: “Towards resolving Cretaceous to Miocene kinematics of the Adria-Europe contact zone in reconstructions: Inferences from a structural study in a critical Dinarides area”
Врста публикације
Рад у часопису
Верзија рада
објављена верзија
Језик рада
енглески
Аутор/и (Милан Марковић, Никола Николић)
Uros Stojadinovic, Nemanja Krstekanić, Liviu Matenco, Tamara Bogdanović
Наслов рада (Наслов - поднаслов)
Towards resolving Cretaceous to Miocene kinematics of the Adria-Europe contact zone in reconstructions: Inferences from a structural study in a critical Dinarides area
Наслов часописа
Terra Nova
Издавач (Београд : Просвета)
Wiley
Година издавања
2022
Сажетак на енглеском језику
One key element in the current debate analysing the Central Mediterranean evolution
is the Cretaceous structure and kinematics of the present-day
oroclinal bent contact between Adria-and Europe-derived continental units in the Dinarides, interpreted in different tectonic reconstructions as a subduction-related thrust system or
a large-scale strike-slip fault zone. We provide a solution to the debate by a structural
and kinematic study in a key area located in central Serbia along the Europe–Adria
orogenic suture of the Sava Zone. The results demonstrate that large-scale, top-SW, in-to
out-of-sequence thrusting is the dominant mechanism that deformed the observed
accretionary wedge-trench sediments during the Late Cretaceous subduction
of the Neotethys Ocean and the ensuing Adria–Europe collision. The subsequent Oligocene–Miocene extension of the Pannonian Basin was associated with opposite-sense rotations of different Sava Zone segments, which created the observed ~80° oroclinal bending.
is the Cretaceous structure and kinematics of the present-day
oroclinal bent contact between Adria-and Europe-derived continental units in the Dinarides, interpreted in different tectonic reconstructions as a subduction-related thrust system or
a large-scale strike-slip fault zone. We provide a solution to the debate by a structural
and kinematic study in a key area located in central Serbia along the Europe–Adria
orogenic suture of the Sava Zone. The results demonstrate that large-scale, top-SW, in-to
out-of-sequence thrusting is the dominant mechanism that deformed the observed
accretionary wedge-trench sediments during the Late Cretaceous subduction
of the Neotethys Ocean and the ensuing Adria–Europe collision. The subsequent Oligocene–Miocene extension of the Pannonian Basin was associated with opposite-sense rotations of different Sava Zone segments, which created the observed ~80° oroclinal bending.
Волумен/том или годиште часописа
34
Број часописа
6
Почетна страна
523
Завршна страна
534
DOI број
10.1111/ter.12618
ISSN број часописа
0954-4879
Кључне речи на српском (одвојене знаком ", ")
/
Кључне речи на енглеском (одвојене знаком ", ")
/
Линк
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12618
Шира категорија рада према правилнику МПНТ
M20
Ужа категорија рада према правилнику МПНТ
М22
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