Turbidity current activity along the flanks of a volcanic edifice: The Mafate volcaniclastic complex, La Réunion Island, Indian Ocean
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- 作者：Aude Mazuela ; aude-mazuel@hotmail.fr" class="auth_mail" title="E-mail the corresponding author ; Emmanuelle Sisavathb ; Nathalie Babonneaua ; Stephan J. Jorryc ; Patrick Bachè ; leryd ; Christophe Delacourta
- 关键词：Deep-sea fan ; Turbidite ; Volcaniclastic ; Land-to-sea transfer ; La Ré ; union Island ; Late Quaternary
- 刊名：Sedimentary Geology
- 出版年：2016
- 出版时间：15 April 2016
- 年：2016
- 卷：335
- 期：Complete
- 页码：34-50
- 全文大小：8391 K
文摘
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We present the first description of the Mafate–Saint-Denis turbidite complex.
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Cores offer a record of the Mafate turbidite system activity over the last 25 ka.
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Turbidite activity occurs during a period dominated by erosional processes on land.
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Two sediment wave fields develop thanks to sandy supplies from turbidity currents.