Highlights A new, more sensitive approach of the Carpathian Foredeep along-arc migration. Developed in three stages the migration was continuous, with two important slowdown periods. Advancing tectonic uplift is the main factor forcing the basinward shifting of the Carpathian Foredeep area. Magmatic and tectonic Carpathian migration processes acted at the same time with the Carpathian Foredeep migration.
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