Supplemental Material: High transient stress in the lower crust: Evidence from dry pseudotachylytes in granulites, Lofoten Archipelago, northern Norway

Kristina Dunkel,Et Al

doi:10.1130/geol.s.12915719

Abstract

List of the localities, description of the methods, supplemental figures detailing the composition of the host rocks (Fig. S1), the distribution and orientation of pseudotachylytes (Fig. S2), the relationship between amphibole and pseudotachylytes (Fig. S3) and the residual pressures of quartz inclusions in garnet (Fig. S4), and supplemental tables on host rock geochemistry (Table S1) and Raman data (Table S2).<br>

Highlights

Figures: Fig. S1: TAS-diagram showing the range of compositions between gabbro and monzonite
Note especially the similarities in composition between host rock and pseudotachylyte for samples HAM-3 and ØL-5
J., Alvaro, M., Miletich, R., and Nestola, F., 2017, A simple and generalised P–T– V EoS for continuous phase transitions, implemented in EosFit and applied to quartz: Contributions to Mineralogy and Petrology, v

Summary

Introduction

Host where Pinc is the residual pressure of the quartz inclusion, G is the shear modulus of the garnet host, V25oC,Pinc is the specific volume of the inclusion at room temperature and residual inc pressure,. 3. Figures: Fig. S1: TAS-diagram showing the range of compositions between gabbro and monzonite.

Results

Conclusion