Tectonic evolution of the Circum-Moesian orocline of the Carpatho-Balkanides: Paleomagnetic constraints

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dc.citation.rankM22
dc.citation.spage102058
dc.citation.volume162
dc.contributor.authorMarton, Emo
dc.contributor.authorCvetkov, Vesna
dc.contributor.authorBanjesević, Miodrag
dc.contributor.authorImre, Gabor
dc.contributor.authorPačevski, Aleksandar
dc.date.accessioned2024-10-16T09:14:04Z
dc.date.available2024-10-16T09:14:04Z
dc.date.issued2024
dc.description.abstractThe areas of the present study in eastern Serbia, the Danubicum and the Timok Magmatic Complex (TMC, part of the Geticum) are situated between the Vardar Zone and Moesia. The first is Moesia derived and thrust over the Geticum during the latest Cretaceous, the second represents the central segment of the subduction related Apuseni-Banat-Timok-Srednogorie (ABTS) metallogenic belt. The new results, based on 18 geographically distributed sampling points (228 field oriented drill cores) imply large CW vertical axis rotations for the Upper Jurassic (Lower Cretaceous) carbonates of the Danubicum and a moderate one for the Upper Cretaceous igneous and sedimentary rocks from the TMC. These, together with earlier published paleomagnetic data provide kinematic constraints to test the circum-Moesian backarc-convex orocline model. The strike test plot clearly documents that it is a progressive arc. The starting situation at the time of the volcanic activity in the metallic belt (90–70 Ma) must have been a generally E-W oriented S segment, continuing in NNW-SSE oriented ABT segments. The present geometry of the circum-Moesian belt, in the context of Miocene paleomagnetic results from the Vardar Zone and the Apuseni Mts, is interpreted as the result of two main tectonic processes. The first is an about 30◦ vertical axis CW rotation which took place in coordination with the Vardar Zone (20–17 Ma). The second is an additional 40–65◦ CW rotation (17–15 Ma) involving also the Danubicum, due to the subduction pull of the E Carpathians in combination with the corner effect of Moesia.
dc.identifier.doi10.1016/j.jog.2024.102058
dc.identifier.issn0264-3707
dc.identifier.urihttps://repozitorijum.tfbor.bg.ac.rs/handle/123456789/5877
dc.language.isoen
dc.publisherElsevier Ltd
dc.rights.licenseARR
dc.rights.uriAll rights reserved
dc.sourceJournal of Geodynamics
dc.subjectApuseni-Banat-Timok-Srednogorie belt
dc.subjectDanubicum
dc.subjectPaleomagnetism
dc.subjectOroclinal bending
dc.titleTectonic evolution of the Circum-Moesian orocline of the Carpatho-Balkanides: Paleomagnetic constraints
dc.typearticle
dc.type.versionpublishedVersion

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