Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone

Márton, Emő; Toljić, Marinko; Cvetkov, Vesna

doi:10.1016/j.jog.2021.101880

Cited by 4 publications

(4 citation statements)

References 53 publications

(75 reference statements)

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“…By restoring the effects of post-20 ma rotations, we reconstruct the Sava zone geometry to an NW-SE-oriented straight suture. [Colour figure can be viewed at wileyonlinelibrary.com] Gora): 40°20° CCW(Lesić et al, 2007) ± BG (Belgrade area): 33°8° CW(Márton et al, 2022) ± RU (Rudnik Mts): 34°20° CW(Lesić et al, 2019) ± KO (Kopaonik Mts): 30°15° CW (Lesić et althese opposite-sense rotations are restored with the higher resolution details of our study, the Sava Zone geometry in the early stages of the Pannonian Basin extension is relatively straight (Figure8b). This is somewhat different when compared with more regional reconstructions, such as the one of van Hinsbergen et al (2020) that still retained around 25° of oroclinal bending at 20 Ma.We interpret the post-20 Ma Sava Zone oroclinal bending to be driven by the retreating Carpathian slab.…”

mentioning

confidence: 57%

“…The present‐day change in the Sava Zone strike taking place between the Fruška Gora and Belgrade area can be correlated with opposite‐sense post‐20 Ma rotations (counter‐clockwise in the E–W segment in Fruška Gora and westwards and clockwise southwards, Figure 8a, Lesić et al, 2007, 2019; Márton et al, 1999, 2022), and with different Late Cretaceous tectonic transport directions in the E–W and N–S oriented segments of the Sava Zone (top‐S and top‐SW, respectively, Toljić et al, 2013, 2018 and this study). These associations indicate that the Sava Zone oroclinal bending occurred during the post‐20 Ma period.…”

Section: Methodological Approachmentioning

confidence: 97%

“…The present-day change in the Sava Zone strike taking place between the Fruška Gora and Belgrade area can be correlated with oppositesense post-20 Ma rotations (counter-clockwise in the E-W segment in Fruška Gora and westwards and clockwise southwards, Figure 8a, Lesić et al, 2007Lesić et al, , 2019Márton et al, 1999Márton et al, , 2022…”

Section: Reconstructing the Geometry Of The Sava Zonementioning

confidence: 99%

“…Horváth et al, 2015). Since the early Miocene, the extension was also associated with significant rotations recorded in different segments of the reactivated Sava Zone (Lesić, Marton, & Cvetkov, 2007; Lesić, Marton, Gajić, Jovanović, & Cvetkov, 2019; Márton, Pavelić, Tomljenović, Pamić, & Márton, 1999; Márton, Toljić, & Cvetkov, 2022).…”

Section: The Evolution Of the Adria–europe Convergence Zone In The St...mentioning

confidence: 99%

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Towards resolving Cretaceous to Miocene kinematics of the Adria–Europe contact zone in reconstructions: Inferences from a structural study in a critical Dinarides area

et al. 2022

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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 oppositesense rotations of different Sava Zone segments, which created the observed ~80° oroclinal bending.

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confidence: 57%