Stress changes during exhumation of a high-pressure nappe (Phyllite-Quartzite unit, Greece): Insights from quartz microstructures and recrystallized grain size statistics

Author:

Xypolias P.ORCID,Lois A.,Aravadinou E.,Gerogiannis N.,Chatzaras V.,Zulauf G.

Publisher

Elsevier BV

Subject

Geology

Reference95 articles.

1. Probing the transition between seismically coupled and decoupled segments along an ancient subduction interface;Angiboust;G-cubed,2015

2. Development and passive exhumation of high-pressure shear zones (Blueschist Unit, Syros): insights from quartz and columnar calcite microstructures;Aravadinou;J. Struct. Geol.,2022

3. What's down there? The structures, materials and environment of deep-seated slow slip and tremor;Behr;Phil. Trans. R. Soc. A,2021

4. Rheological evolution of a Mediterranean subduction complex;Behr;J. Struct. Geol.,2013

5. Brittle faults are weak, yet the ductile middle crust is strong: implications for lithospheric mechanics;Behr;Geophys. Res. Lett.,2014

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