Changes in electrical resistivity track changes in tectonic plate coupling

Interplate coupling on the Hikurangi subduction margin along the east coast of New Zealand's North Island changes north to south from almost uncoupled to locked. Clay‐rich sediments and aqueous fluids at the subduction interface have been invoked as key factors in the frictional processes that...

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Veröffentlicht in:	Geophysical research letters 2013-10, Vol.40 (19), p.5029-5033
Hauptverfasser:	Heise, Wiebke, Caldwell, T. Grant, Bertrand, Edward A., Hill, Graham J., Bennie, Stewart L., Ogawa, Yasuo
Format:	Artikel
Sprache:	eng
Schlagworte:	Clay Electrical resistivity Geophysics magnetotellurics plate coupling Plate tectonics Sediments Seismology slow slip subduction
Online-Zugang:	Volltext
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