Data/hora: 04/06/2024 01:37:56

Provedor de dados: 	5	
País: 	France	
Título: 	Facteurs de contrôle sur le fonctionnement du système turbiditique du Rhône depuis le Dernier Maximum Glaciaire	
Autores: 	Lombo Tombo, Swesslath.	
Data: 	2015-07-03	
Ano: 	2015	
Palavras-chave: 	Hyperpycnite; Turbidites; Système turbiditique du Rhône; Facteurs de contrôle; Niveau marin; Climat; Morphologie; Golfe du Lion; Méditerranée occidentale; Hyperpycnites; Turbidites; Rhone turbidite system; Control factors; Sea level; Climate; Morphology; Gulf of Lions; Western Mediterranean.	
Resumo: 	Turbidite systems are accumulations of fluvial sediment on the continental margins. They are mainly made of « turbidites » deposited after the flow of turbidity currents inside submarine canyons and channels. Their structure and composition are controlled by global and regional environmental changes such as sea level and climate. The two fundamental parameters that govern their functioning are the production of sediment in the river watersheds and the capability and reactivity of the transfer to the turbidite system. In this work we show that for the last 24,000 years the functioning of the Rhone turbidite system has shown rapid changes under the control of sea level and sediment production fluctuations. Our results are based on a millennial time-scale chrono-stratigraphy obtained on turbidites collected in sediment cores during the RHOSOS and other cruises.	
Tipo: 	Text	
Idioma: 	Francês	
Identificador: 	http://archimer.ifremer.fr/doc/00274/38505/37013.pdf

http://archimer.ifremer.fr/doc/00274/38505/	
Editor: 	Université de Perpignan via Domitia	
Formato: 	application/pdf	
Fonte: 	2015 Université de Perpignan

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