Twinning and partial melting as early weakening processes in plagioclase at high pressure: insights from Holsnøy (Scandinavian Caledonides, Norway)
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00410-023-01998-x.pdf
Reference138 articles.
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2. Andersen TB, Corfu F, Labrousse L, Osmundsen PT (2012) Evidence for hyperextension along the pre-Caledonian margin of Baltica. J Geol Soc 169(5):601–612. https://doi.org/10.1144/0016-76492012-011
3. Austrheim H (1987) Eclogitization of lower crustal granulites by fluid migration through shear zones. Earth Planet Sci Lett 81(2–3):221–232. https://doi.org/10.1016/0012-821X(87)90158-0
4. Austrheim H (1991) Eclogite formation and dynamics of crustal roots under continental collision zones. Terra Nova 3(5):492–499. https://doi.org/10.1111/j.1365-3121.1991.tb00184.x
5. Austrheim H (2013) Fluid and deformation induced metamorphic processes around Moho beneath continent collision zones: Examples from the exposed root zone of the Caledonian mountain belt, W-Norway. Tectonophysics 609:620–635. https://doi.org/10.1016/j.tecto.2013.08.030
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