Relationships between the microstructural evolution and the rheology of talc at elevated pressures and temperatures

We conducted triaxial compression experiments to investigate the effects of pressure, temperature and strain rate on the rheology of talc rocks. The tests were carried out at T from 25 to 860 °C, P from 0.1 to 300 MPa, and ε˙ from 0.3 to 30 × 10 − 5  s − 1 . In addition to being very weak, there are...

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Veröffentlicht in:	Earth and planetary science letters 2008-04, Vol.268 (3), p.463-475
Hauptverfasser:	Escartín, J., Andreani, M., Hirth, G., Evans, B.
Format:	Artikel
Sprache:	eng
Schlagworte:	dehydration Earth Sciences Environmental Sciences Geophysics Global Changes Physics rheology rock mechanics Sciences of the Universe subduction talc
Online-Zugang:	Volltext
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