THE FOREDEEPS OF THE NORTHERN ADRIATIC MARGIN: EVIDENCE OF DIACHRONEITY IN DEFORMATION OF THE SOUTHERN ALPS
The evolution of the foredeeps which developed on the northern Adriatic foreland took piace in a regime of oblique convergence. From the Late Oligocene onwards much compression in the Southern Alps must have been the compressional component of dextral transpression along the Insubric Line, as sugge...
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| Format: | Article |
| Language: | English |
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Università degli Studi di Milano
2017-08-01
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| Series: | Rivista Italiana di Paleontologia e Stratigrafia |
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| Online Access: | https://riviste.unimi.it/index.php/RIPS/article/view/9043 |