0000000000224903

AUTHOR

Emilien Oliot

0000-0002-0370-990x

showing 1 related works from this author

How does shear zone nucleate? An example from the Suretta nappe (Swiss Eastern Alps)

2016

In order to address the question of the processes involved during shear zone nucleation, we present a petro-structural analysis of millimetre-scale shear zones within the Roffna rhyolite (Suretta nappe, Eastern central Alps). Field and microscopic evidences show that ductile deformation is localized along discrete fractures that represent the initial stage of shear zone nucleation. During incipient brittle deformation, a syn-kinematic metamorphic assemblage of white mica + biotite + epidote + quartz precipitated at ca. 8.5 ± 1 kbar and 480 ± 50 °C that represent the metamorphic peak conditions of the nappe stacking in the continental accretionary wedge during Tertiary Alpine subduction. The…

[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics010504 meteorology & atmospheric sciencesAlpsNucleationDiffusion creepGeologyBrittle-ductile transition[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics010502 geochemistry & geophysicsSuretta nappe01 natural sciencesShear zone nucleationNappeBrittlenessShear (geology)Deformation mechanismShear zonePetrologyFluid-rock interactionGeomorphologyGeology0105 earth and related environmental sciencesGrain Boundary Sliding
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