Thèse de doctorat : Université de Fribourg, 2011 ; no. 1733.
The Greater Caucasus is Europe’s largest and highest mountain belt and results from the inversion of the Mesozoic Greater Caucasus back-arc-type basin due to the collision of Arabia and Eurasia. The orogenic processes that led to the present mountain chain started in early Tertiary, accelerated during the Plio- Pleistocene, and are still active nowadays. The Eastern Greater Caucasus (EGC) is...
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In: Geological Society, London, Special Publications, 2010, vol. 340, p. 261-280
The Greater Caucasus is Europe's highest mountain belt and results from the inversion of the Greater Caucasus back-arc-type basin due to the collision of Arabia and Eurasia. The orogenic processes that led to the present mountain chain started in the Early Cenozoic, accelerated during the Plio-Pleistocene, and are still active as shown from present GPS studies and earthquake distribution. The...
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In: Actes du 12e Congrès national de spéléologie : La Vallée de Joux, 15,16,17 septembre 2007, 148
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In: Stalactite 54/1, 2004, p. 39-47
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In: Actes du 12e Congrès suisse de Spéléologie, 2007, p. 148-154.
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