The transition between the two major Permian tectono-stratigraphic cycles in the central Southern Alps: results from facies analysis and U/Pb geochronology

The Val Daone Conglomerate (VDC) is a continental clastic unit that crops out eastwards of the central Southern Alps, from the NE sector of the Collio Basin to the W as far as the Tione Basin to the E. This significant but as yet relatively unknown formation lies just above the regional unconformity...

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Veröffentlicht in:	International journal of earth sciences : Geologische Rundschau 2013-07, Vol.102 (5), p.1181-1202
Hauptverfasser:	Gretter, Nicola, Ronchi, Ausonio, Langone, Antonio, Perotti, Cesare R.
Format:	Artikel
Sprache:	eng
Schlagworte:	Alluvial fans Earth and Environmental Science Earth Sciences Geochemistry Geological time Geology Geophysics Geophysics/Geodesy Lava Mineral Resources Mountains Permian Plate tectonics Pollen Review Article Sandstone Sedimentology Stratigraphy Structural Geology Unconformity Volcanic rocks
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