The Borghetto d'Arroscia sequence begins with a little known basel post, followed by two lithostratigraphic units: the M. Bignone Quartzites (Paleocene?-Eocene?) and the Ubaga Limestones (Eocene). Three deformation phases affected the tectonic evolution of the Borghetto d'Arroscia element. The first two phases are vergent outwards. The former (F 1) is characterized by S-vergent recumbent folds, the latter (F 1b) gives cut planes slightly dipping, forming the overthrust surface to the same direction. The third phase (F 2) is retrovergent and does not change the general structural setting already reached.-from English summary

Aspects of stratigraphy and structure of the Borghetto d'Arroscia sequence, Maritime Alps. [Aspetti stratigrafici e strutturali dell'elemento di Borghetto d'Arroscia (Alpi marittime).]

SENO, SILVIO
1983-01-01

Abstract

The Borghetto d'Arroscia sequence begins with a little known basel post, followed by two lithostratigraphic units: the M. Bignone Quartzites (Paleocene?-Eocene?) and the Ubaga Limestones (Eocene). Three deformation phases affected the tectonic evolution of the Borghetto d'Arroscia element. The first two phases are vergent outwards. The former (F 1) is characterized by S-vergent recumbent folds, the latter (F 1b) gives cut planes slightly dipping, forming the overthrust surface to the same direction. The third phase (F 2) is retrovergent and does not change the general structural setting already reached.-from English summary
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11571/454348
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