Subseismic to Seismic Slip in Smectite Clay Nanofoliation

Autor:	Aretusini, S., Plümper, O., Spagnuolo, E., Di Toro, G., Structural geology and EM, Structural geology & tectonics
Přispěvatelé:	Structural geology and EM, Structural geology & tectonics
Jazyk:	angličtina
Rok vydání:	2019
Předmět:	deformation processes earthquake high velocity friction microstructure 010504 meteorology & atmospheric sciences Slip (materials science) 01 natural sciences High Strain Deformation Zones Radio Science Structural Geology Geochemistry and Petrology Earthquake Dynamics Earth and Planetary Sciences (miscellaneous) Geodesy and Gravity Petrology Slipping Seismology Earthquake Interaction Forecasting and Prediction Research Articles 0105 earth and related environmental sciences Subduction Creep and Deformation Landslide Mineral Physics Seismic Cycle Related Deformations Geophysics Interferometry Creep 13. Climate action Space and Planetary Science Trench Seismicity and Tectonics Grain boundary Clay minerals Geology Chemistry and Physics of Minerals and Rocks/Volcanology Research Article
Zdroj:	Journal of Geophysical Research. Solid Earth Journal of Geophysical Research: Solid Earth, 124(7), 6589
ISSN:	2169-9313
Popis:	Smectite clays are the main constituent of slipping zones found in subduction zone faults at shallow depth (e.g. Key Points Nanofoliations develop at subseismic to seismic slip rates in partly water saturated smectite fault gougesNanofoliations may deform by frictional slip in smectite water‐lubricated basal planes and grain boundariesStrain localized nanofoliations can be diagnostic of past slip events at rates larger than 0.01 m/s in natural fault rocks
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_dedup___::548b0c33753c2d6b4ad6f1de855e3036 http://hdl.handle.net/11577/3308706 Zobrazit plný text záznamu Plný text