LE RELAZIONI TRA LE ARENARIE DI SARNICO (CONIACIANO) E LE UNITA' CENOMANIANO-TURONIANE NELL'AREA DI CAPRIOLO - CORNO PENDITA (BS) (BACINO LOMBARDO, ALPI MERIDIONALI)

Authors

  • R. BERSEZIO
  • L. MENSINI

DOI:

https://doi.org/10.13130/2039-4942/8940

Keywords:

Cretaceous, Lombardy Basin, Southern Alps, stratigraphy, unconformities.

Abstract

The Cenomanian-Coniacian units of the Capriolo - Corno Pendita area belong to the eastern margin of the Lombardy Basin. The Coniacian turbidite sandstone lithosome (Arenarie di Sarnico) unconformably overlies the Cenomanian-Turonian units. The unconformity should be due to slumping and sliding during Late Turonian time. The Arenarie di Sarnico seal the geometries related to the Cenomanian - Turonian synsedimentary tectonic. Evidences for this activity are provided by slumpings and chaotic beds (Early-Late Cenomanian) and by unconformities predating the submarine erosion phase.

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Issue

Vol. 98 No. 1 (1992)

Section

Articles

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The journal allow the author(s) to hold the copyright without restrictions.

How to Cite

“LE RELAZIONI TRA LE ARENARIE DI SARNICO (CONIACIANO) E LE UNITA’ CENOMANIANO-TURONIANE NELL’AREA DI CAPRIOLO - CORNO PENDITA (BS) (BACINO LOMBARDO, ALPI MERIDIONALI)” (1992) RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA , 98(1). doi:10.13130/2039-4942/8940.