Semibrittle seismic deformation in high-temperature mantle mylonite shear zone along the Romanche transform fault-Reference-Cited by-同舟云学术

Semibrittle seismic deformation in high-temperature mantle mylonite shear zone along the Romanche transform fault

Author:

Yu Zhiteng¹^ORCID,Singh Satish C.¹^ORCID,Gregory Emma P. M.¹^ORCID,Maia Marcia²³^ORCID,Wang Zhikai¹^ORCID,Brunelli Daniele⁴⁵^ORCID

Affiliation:

1. Université de Paris, Institut de Physique du Globe de Paris, CNRS, Paris, France.

2. CNRS-Université de Bretagne Occidentale, IUEM, France.

3. Laboratoire Géosciences Océan, CNRS-UBO UMR 6538, Institut Universitaire Européen de la Mer Rue Dumont d’Urville, 29280 Plouzané France.

4. Università di Modena e Reggio Emilia, Modena, Italy.

5. Institute for Marine Sciences ISMAR-CNR, Italy.

Abstract

Deep microseismicity occurs in high-temperature ductile mantle mylonite shear zones resulting from semibrittle fracturing.

Funder

European Research Council

Interdisciplinary graduate school for the blue planet

Italian Programma di Rilevante Interesse Nazionale

French government under the program "Investissements d’Avenir”

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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