2002
DOI: 10.5194/smsps-3-41-2002
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The Pannonian basin: Dynamic modelling of the transition from passive to active rifting

Abstract: Abstract. We examine a number of first order features of Pannonian basin evolution in terms of the feedback relation between passive far-field induced extension and active Raleigh-Taylor instable upwelling of the asthenosphere. We show that active mantle upwelling following a phase of passive extension are viable mechanisms explaining the Pannonian basin formation. The dynamic interplay between far-field driven passive extension and active thinning of the mantle lithosphere by convective upwelling beneath the … Show more

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Cited by 15 publications
(19 citation statements)
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“…Middle to Late Miocene compressional structures are widespread in the basin, and are also indicated by microtectonic (Ciulavu, 1999;Huismans, 1999) and seismic data (De Broucker et al, 1998;Ciulavu, 1999; our data). However, most faults stop in the salt-layer, indicating that the salt represented a major decoupling horizon, between the pre-salt and post-salt succession.…”
Section: Middle Mid-miocene (Late Badenian To Early Sarmatian): Tst4-mentioning
confidence: 79%
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“…Middle to Late Miocene compressional structures are widespread in the basin, and are also indicated by microtectonic (Ciulavu, 1999;Huismans, 1999) and seismic data (De Broucker et al, 1998;Ciulavu, 1999; our data). However, most faults stop in the salt-layer, indicating that the salt represented a major decoupling horizon, between the pre-salt and post-salt succession.…”
Section: Middle Mid-miocene (Late Badenian To Early Sarmatian): Tst4-mentioning
confidence: 79%
“…Several contrasting data have been published. Huismans et al (1997), Huismans (1999), and Ciulavu (1999) support the existence of a small scale, east-west oriented, early Mid-Miocene tensional phase in the Transylvanian Basin. However, no major regional faults have been identified so far.…”
Section: Early Mid-miocene (Early To Mid-badenian): Tst1-lst4mentioning
confidence: 99%
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