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In the Piz da Peres area (Valdaora-Olang, Pusteria Valley, Italy) an Anisian succession is exposed,A redefinition of the lithostratigraphy is made, and the presence of three terrigenous units of different ages (Piz da Peres Conglomerate, Voltago Conglomerate and Richthofen Conglomerate), as well as two carbonate platforms (Upper Serla Formation and Contrin Formation), is documented. This stratigraphic setting correlates well with other Anisian sections outcropping in the Dolomites and in the Recoaro area.Using sequence stratigraphy as an integrated approach, four Anisian depositional sequences are identified. Preliminary results indicate that these sequences can be recognized throughout the Dolomites and the Recoaro area, and might even extend to the Southern Alps.

The Piz da Peres section (Valdaora-Olang, Pusteria Valley, Italy). A reappraisal of the Anisian stratigraphy in the Dolomites

GIANOLLA, Piero;
1992

Abstract

In the Piz da Peres area (Valdaora-Olang, Pusteria Valley, Italy) an Anisian succession is exposed,A redefinition of the lithostratigraphy is made, and the presence of three terrigenous units of different ages (Piz da Peres Conglomerate, Voltago Conglomerate and Richthofen Conglomerate), as well as two carbonate platforms (Upper Serla Formation and Contrin Formation), is documented. This stratigraphic setting correlates well with other Anisian sections outcropping in the Dolomites and in the Recoaro area.Using sequence stratigraphy as an integrated approach, four Anisian depositional sequences are identified. Preliminary results indicate that these sequences can be recognized throughout the Dolomites and the Recoaro area, and might even extend to the Southern Alps.
1992
DE ZANCHE, V.; Franzin, A.; Gianolla, Piero; MIETTO P., SIORPAES C.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11392/461803
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