The Addition of Felsic Sediments to the Lower Continental Crust During the Variscan Orogeny

The Addition of Felsic Sediments to the Lower Continental Crust During the Variscan Orogeny

Abstract Lower crustal metasedimentary xenoliths (garnet‐sillimanite granulites) from the Bournac breccia pipe in the Massif Central, France, provide a robust example of sediments transported to depth and incorporated into stable lower continental crust during a collisional orogeny. Dates for detrit...

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Bibliografiske detaljer
Main Authors: M. F. Ringwood, S. E. Ortner, R. L. Rudnick
Format: Article
Sprog:English
Udgivet: Wiley 2025-01-01
Serier:Geochemistry, Geophysics, Geosystems
Fag:
petrochronology
lower crustal metasediments
continental crust
xenoliths
Online adgang:https://doi.org/10.1029/2024GC011843

Internet

https://doi.org/10.1029/2024GC011843

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