On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)

The French Riviera has witnessed a succession of E-W trending compressions during the Oligocene period and a N-S trending compression during the Mio-Pliocene. The presence of the Ligurian Sea and drifting of the Corsica block are due to a NW-SE trending Oligo-Miocene extension. The markers of each c...

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Main Author: Lionel Sonnette
Format: Article
Language:English
Published: Springer 2016-04-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/pdf/v272p203.pdf
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author Lionel Sonnette
author_facet Lionel Sonnette
author_sort Lionel Sonnette
collection DOAJ
description The French Riviera has witnessed a succession of E-W trending compressions during the Oligocene period and a N-S trending compression during the Mio-Pliocene. The presence of the Ligurian Sea and drifting of the Corsica block are due to a NW-SE trending Oligo-Miocene extension. The markers of each compression are recognizable from the geological maps and they have been studied extensively in the literature. However, markers of the Ligurian Basin opening have never been described on land in the French Riviera. The structural study of the Cap-Ferrat Peninsula, at the South edge of the Nice arc, shows normal and inverse fault clusters. Their chronological relationships and the main trend of their respective stress tensors agree with the different known tectonic events and allow identification of the missing Oligo-Miocene extension on land.
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spelling doaj.art-3bfbcc68080d41bd85c1d19388efba2f2022-12-22T02:26:13ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08391017-08392016-04-0127218119310.3319/TAO.2015.12.04.01(TT)1337On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)Lionel SonnetteThe French Riviera has witnessed a succession of E-W trending compressions during the Oligocene period and a N-S trending compression during the Mio-Pliocene. The presence of the Ligurian Sea and drifting of the Corsica block are due to a NW-SE trending Oligo-Miocene extension. The markers of each compression are recognizable from the geological maps and they have been studied extensively in the literature. However, markers of the Ligurian Basin opening have never been described on land in the French Riviera. The structural study of the Cap-Ferrat Peninsula, at the South edge of the Nice arc, shows normal and inverse fault clusters. Their chronological relationships and the main trend of their respective stress tensors agree with the different known tectonic events and allow identification of the missing Oligo-Miocene extension on land. http://tao.cgu.org.tw/pdf/v272p203.pdf Brittle tectonicFaultStress tensorFrench RivieraLigurian Basin
spellingShingle Lionel Sonnette
On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)
Terrestrial, Atmospheric and Oceanic Sciences
Brittle tectonic
Fault
Stress tensor
French Riviera
Ligurian Basin
title On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)
title_full On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)
title_fullStr On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)
title_full_unstemmed On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)
title_short On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)
title_sort on land evidence of ligurian margin normal faults at st jean cap ferrat france
topic Brittle tectonic
Fault
Stress tensor
French Riviera
Ligurian Basin
url http://tao.cgu.org.tw/pdf/v272p203.pdf
work_keys_str_mv AT lionelsonnette onlandevidenceofligurianmarginnormalfaultsatstjeancapferratfrance