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...

पूर्ण विवरण

ग्रंथसूची विवरण
मुख्य लेखकों:	M. F. Ringwood, S. E. Ortner, R. L. Rudnick
स्वरूप:	लेख
भाषा:	English
प्रकाशित:	Wiley 2025-01-01
श्रृंखला:	Geochemistry, Geophysics, Geosystems
विषय:	petrochronology lower crustal metasediments continental crust xenoliths
ऑनलाइन पहुंच:	https://doi.org/10.1029/2024GC011843

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