Rheological evolution of a Mediterranean subduction complex

We use field and microstructural observations, coupled to previously published P-T-time histories, to track the rheological evolution of an intracontinental subduction complex exposed in the Betic Cordillera in the western Mediterranean region. The body of rock we focus on, known as the Nevado-Filab...

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Veröffentlicht in:	Journal of structural geology 2013-09, Vol.54, p.136-155
Hauptverfasser:	Behr, Whitney Maria, Platt, John Paul
Format:	Artikel
Sprache:	eng
Schlagworte:	Betic Cordillera Continental subduction Dislocation creep Grain boundary sliding Mylonites Paleopiezometry Pressure solution Quartzite flow law Stress in subduction zones Subduction complex
Online-Zugang:	Volltext
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