Spatiotemporal Characterization of Smectite‐to‐Illite Diagenesis in the Nankai Trough Accretionary Prism Revealed by Samples From 3 km Below Seafloor-Reference-Cited by-同舟云学术

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Spatiotemporal Characterization of Smectite‐to‐Illite Diagenesis in the Nankai Trough Accretionary Prism Revealed by Samples From 3 km Below Seafloor

Published:2019-02 Issue:2 Volume:20 Page:933-951
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Hüpers A.¹,Grathoff G.²,Warr L. N.²,Wemmer K.³,Spinelli G.⁴^ORCID,Underwood M. B.⁴^ORCID

Affiliation:

1. MARUM—Center for Marine Environmental SciencesUniversity of Bremen Bremen Germany

2. Institute of Geography and GeologyUniversity of Greifswald Greifswald Germany

3. Geoscience CentreUniversity of Göttingen Göttingen Germany

4. Earth and Environmental Science DepartmentNew Mexico Institute of Mining and Technology Socorro NM USA

Funder

Consortium for Ocean Leadership

Deutsche Forschungsgemeinschaft

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GC008015

Reference89 articles.

1. Density, porosity, and compaction of sedimentary rocks;Athy L. F.;AAPG Bulletin,1930

2. A simplified analysis of parameters controlling dewatering in accretionary prisms

3. Influence of kinetics on the smectite to illite transition in the Barbados accretionary prism

4. Deformation of the Nankai Trough inner accretionary prism: The role of inherited structures

5. Compositional and fluid pressure controls on the state of stress on the Nankai subduction thrust: A weak plate boundary

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