Stratigrafia sequenziale del Terziario nella Catena del Monte Baldo (Provincie di Verona e Trento)
The Tertiary succession outcropping on the eastern side of the Garda lake (M. BAldo, M: Brione, Val di gresta etc.) have been studied by means of facies analysis and biostratigraphy (Larger and planktonic foraminifera). As a result, the paleogeographic and structural evolution of the western margin...
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| Format: | Article in Journal/Newspaper |
| Language: | Italian |
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1989
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| Online Access: | http://hdl.handle.net/11392/1736678 |
| Summary: | The Tertiary succession outcropping on the eastern side of the Garda lake (M. BAldo, M: Brione, Val di gresta etc.) have been studied by means of facies analysis and biostratigraphy (Larger and planktonic foraminifera). As a result, the paleogeographic and structural evolution of the western margin of the Lessini Shelf has been reconstructed. |
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