Institut des Sciences de la Terre d'Orléans, UMR CNRS 6113,
Université d'Orléans, Campus Géosciences, 1A, rue de la
Férollerie, 45071 Orléans cedex 2, France
Muriel Andreani
Laboratoire de Géologie de Lyon, École Normale Supérieure
de Lyon et Université Claude Bernard Lyon 1, UMR 5276 CNRS, 2 rue
Raphaël Dubois, 69622 Villeurbanne cedex, France
Anne-Marie Boullier
CNRS, ISTerre, Université Grenoble Alpes, 38041 Grenoble,
France
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EndNote: 39
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Total article views: 1,888 (including HTML, PDF, and XML)
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1,563
285
40
1,888
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HTML: 1,563
PDF: 285
XML: 40
Total: 1,888
BibTeX: 26
EndNote: 35
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Cumulative views and downloads
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Total article views: 650 (including HTML, PDF, and XML)
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406
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650
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HTML: 406
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Total: 650
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Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 2,538 (including HTML, PDF, and XML)
Thereof 2,429 with geography defined
and 109 with unknown origin.
Total article views: 1,888 (including HTML, PDF, and XML)
Thereof 1,827 with geography defined
and 61 with unknown origin.
Total article views: 650 (including HTML, PDF, and XML)
Thereof 602 with geography defined
and 48 with unknown origin.
Sediments accumulated in accretionary prisms are deformed by the compression imposed by plate subduction. Here we show that deformation of the sediments transforms some minerals in them. We suggest that these mineral transformations are due to the proliferation of microorganisms boosted by deformation. Deformation-enhanced microbial proliferation may change our view of sedimentary and tectonic processes in subduction zones.
Sediments accumulated in accretionary prisms are deformed by the compression imposed by plate...