 |
Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie |  |
Journal articles
Anatectic melt inclusions in ultra‐high temperature granulites
Abstract : Partial melting up to ultra-high temperature (UHT) conditions is one of the major processes for the geochemical differentiation and reworking of the mid-to lower continental crust, with relevant implications on its rheological behaviour. UHT granulites from the Gruf Complex (Central Alps) display garnet and sapphirine porphyroblasts containing a variety of primary melt inclusions. Typically, melt inclusions in garnets occur as glassy and polycrystalline
https://hal.archives-ouvertes.fr/hal-02959289
Contributor : Laurent Remusat <>
Submitted on : Thursday, December 24, 2020 - 7:23:25 PM
Last modification on : Saturday, January 9, 2021 - 3:40:12 AM
Contributor : Laurent Remusat <>
Submitted on : Thursday, December 24, 2020 - 7:23:25 PM
Last modification on : Saturday, January 9, 2021 - 3:40:12 AM
File
OG_MI_Gruf_v3-LR.pdf
Files produced by the author(s)