Thermobarometric constraints on pressure variations across the Plattengneiss shear zone of the Eastern Alps: Implications for exhumation models during Eoalpine subduction
Forward and inverse mineral equilibria modelling of metapelitic rocks in the hangingwall and footwall of the Plattengneiss, a major shear zone in the Eastern Alps, are used to constrain their tectonometamorphic evolution and assess models for their exhumation. Forward (pseudosection) modelling of tw...
Main Authors: | , , , , |
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Format: | Journal Article |
Published: |
Wiley - Blackwell
2014
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Subjects: | |
Online Access: | http://hdl.handle.net/20.500.11937/3033 |