Source tracing of detrital serpentinite in the Oligocene molasse deposits from the western Alps (Barrême basin): Implications for relief formation in the internal zone

Geological Magazine

Volumn 149, Issue 5, 2012, Pages 841-856

  Schwartz, S ^a   Guillot, S ^a   Tricart, P ^a   Bernet, M ^a   Jourdan, S ^a   Dumont, T ^a   Montagnac, G ^b  

^a UNIVERSITÉ GRENOBLE ALPES   (France)

^b CNRS   (France)

Author keywords

Barr me basin; Raman spectroscopy; serpentinite pebbles; source tracing; western Alps

Indexed keywords

KAOLINITE; MAGNESITE; RAMAN SPECTROSCOPY; SEDIMENT TRANSPORT; SERPENTINE; TEMPERATURE;

HIGH TEMPERATURE; LOW TEMPERATURES; SERPENTINITE; SERPENTINIZED PERIDOTITES; SOURCE TRACING; STRUCTURAL DATA; TRANSPORT DIRECTION; WESTERN ALPS;

DEPOSITS;

ANTIGORITE; DETRITAL DEPOSIT; LIZARDITE; MIOCENE; MOLASSE; OLIGOCENE; OPHIOLITE; PEBBLE; RAMAN SPECTROSCOPY; SEDIMENT TRANSPORT; SERPENTINITE; SUBDUCTION; THERMOCHRONOLOGY; UPLIFT;

ALPES DE HAUTE PROVENCE; ALPS; BARREME BASIN; FRANCE; PROVENCE-ALPES-COTE D'AZUR; WESTERN ALPS;

EID: 84862267223     PISSN: 00167568     EISSN: 14695081     Source Type: Journal    
DOI: 10.1017/S0016756811001105     Document Type: Article

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