Activation of dissolution-precipitation creep causes weakening and viscous behaviour in experimentally-deformed antigorite

Antigorite occurs at seismogenic depth along plate boundary shear zones, particularly in subduction and oceanic transform settings, and has been suggested to control a low strength bulk rheology. To constrain dominant deformation mechanisms, we perform hydrothermal ring-shear experiments on antigori...

Ausführliche Beschreibung

Bibliographische Detailangaben

1. Verfasser:	Niemeijer, André Rik
Format:	Dataset
Sprache:	eng
Schlagworte:	Antigorite EPOS Friction hydrothermal ring-shear experiments low strength bulk rheology multi-scale laboratories plate boundary shear zones Powder Mixture Rock and melt physical properties rock and melt physics properties Rotary Shear seismogenic depth subduction and oceanic transform settings
Online-Zugang:	Volltext bestellen
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!