Geodynamics of Rifting 1992
DOI: 10.1016/b978-0-444-89912-5.50017-x
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Tertiary evolution of the Intra-Carpathian area: a model

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Cited by 427 publications
(392 citation statements)
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“…An over view of the tec tonic set ting and re gional geo logic evo lu tion of the Pannonian Ba sin is given by Huismans et al (2002) us ing data from Bergerat (1989), Csontos et al (1991), Ratschbacher et al (1993), Horváth (1995, Bergerat (1995), Csontos (1995), Fodor (1995), Hippolyte and Sandulescu (1996), Sachsenhofer (1996), Sachsenhofer et al (1997), Huis mans et al (1997), Maþenco (1997), Peresson and Decker (1997a, b), Sanders (1998), Fodor et al (2000) and Huismans and Bertotti (2002). Ac cord ing to Huismans et al (2002), the Early to Late Mio cene ex ten sion led to a sig nif i cant thin ning of the litho sphere (down to 60 to 80 km with a crustal thick ness of ~22.5 to 30 km) with high gra di ents of litho sphere thick ness in the east ern and west ern ba sin bor der re gions.…”
Section: Geological/tectonic Setting Of the Alpine-carpathian-pannonimentioning
confidence: 99%
“…An over view of the tec tonic set ting and re gional geo logic evo lu tion of the Pannonian Ba sin is given by Huismans et al (2002) us ing data from Bergerat (1989), Csontos et al (1991), Ratschbacher et al (1993), Horváth (1995, Bergerat (1995), Csontos (1995), Fodor (1995), Hippolyte and Sandulescu (1996), Sachsenhofer (1996), Sachsenhofer et al (1997), Huis mans et al (1997), Maþenco (1997), Peresson and Decker (1997a, b), Sanders (1998), Fodor et al (2000) and Huismans and Bertotti (2002). Ac cord ing to Huismans et al (2002), the Early to Late Mio cene ex ten sion led to a sig nif i cant thin ning of the litho sphere (down to 60 to 80 km with a crustal thick ness of ~22.5 to 30 km) with high gra di ents of litho sphere thick ness in the east ern and west ern ba sin bor der re gions.…”
Section: Geological/tectonic Setting Of the Alpine-carpathian-pannonimentioning
confidence: 99%
“…The Apuseni-Banat-Timok-Srednogorie (ABTS) belt represents a continental margin magmatic arc, whose tectonic evolution broadly relates to subduction processes prior to the Upper Cretaceous collision events (Ciobanu et al, 2002). Paleomagnetic studies show that the present sinusoidal L shape of the belt is a result of an~80°clockwise rotation of the Apuseni Mountains and Banat sectors during the Tertiary (Patrascu et al, 1992(Patrascu et al, , 1994Csontos, 1995;Fügenschuh and Schmid, 2005).…”
Section: Apuseni-banat-timok-srednogorie Belt and Srednogorie Zonementioning
confidence: 99%
“…The Paleogene was a period of tectonic quiescence. During the Neogene the microcontinents collided en bloc with the European continental margin [Burchfiel, 1980;Sandulescu, 1988;Csontos, 1995 The Moldavides occupy the main part of the orogen and are situated on its most eastern side. The nappe systems are made up of flysch sediments with stratigraphic ages ranging from late Early Cretaceous in the internal nappes to middle Miocene in the more external nappes.…”
Section: Regional Geological Settingmentioning
confidence: 99%