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Mineral and fluid thermobarometry within the Variscan shearzone of Monteferro-El Rosal (NW Galicia, Spain): a preliminary investigation

✍ Scribed by Hébert


Book ID
104463153
Publisher
John Wiley and Sons
Year
1997
Tongue
English
Weight
256 KB
Volume
9
Category
Article
ISSN
0954-4879

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✦ Synopsis


The Monteferro El Rosal shear zone is characterized by an intense ductile deformation produced during the third phase of the Variscan orogeny. The petrology of the metasediments and the study of the fluid inclusions from synkinematic andalusite‐bearing quartz veins indicate that the major Variscan phase of deformation occurred at around 2. 5–4 kbar and 565 ± 25°C.