Referenza:
▪ Cesare, B., Parisatto, M., Mancini, L., Peruzzo, L., Franceschi, M., Tacchetto, T., Reddy, S.M., Spiess, R. Nestola, F., Marone, F. (2020): Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet. Earth and Planetary Sciences Letters, 555, 116708.
Abstract:
Sheltered inside crystals, mineral inclusions preserve crucial information on the geological history of our planet. These inclusions allow estimation of the pressure and temperature trajectories of metamorphic rocks, but also can tell about rock mineralogy, provenance, and geodynamic and petrogenetic processes. This information is recovered under the axiom that mineral inclusions have remained immutable objects that do not change shape after their entrapment. Conversely, we show that post-entrapment shape modifications do occur in high-T rocks from granulite-facies conditions. Here we analyze the shape and orientation of quartz inclusions within garnet, a common metamorphic mineral. Our data reveal a progressive change in shape from irregularly-shaped forms in rocks formed at T<550 °C, to combined dodecahedron and icositetrahedron geometries imposed by the host garnet in granulites equilibrated at T>750 °C. Lack of fluid at the quartz-garnet phase boundary indicates that inclusion shape change occurs by thermally-induced grain boundary diffusion, driven by the minimization of the surface energy of the host-inclusion system. Since inclusions acquire a negative crystal shape after entrapment, our discovery redefines the conceptual framework for the application of elastic thermobarometry, and motivates a reevaluation of the criteria for mineral inclusion syngenesis in metamorphic rocks.
Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet
- Marco E. Ciriotti
- Messaggi: 30668
- Iscritto il: ven 25 giu, 2004 11:31
- Località: via San Pietro, 55 I-10073 Devesi/Cirié TO - Italy
- Contatta:
Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet
Marco E. Ciriotti
«Things are interesting only in so far as they relate themselves to other things»
«Things are interesting only in so far as they relate themselves to other things»
-
- Messaggi: 546
- Iscritto il: sab 27 apr, 2013 13:32
- Marco E. Ciriotti
- Messaggi: 30668
- Iscritto il: ven 25 giu, 2004 11:31
- Località: via San Pietro, 55 I-10073 Devesi/Cirié TO - Italy
- Contatta:
Re: Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet
Sì, certo.
Te lo passo non appena lo avrò dagli autori.
Eccolo qui allegato.
Te lo passo non appena lo avrò dagli autori.
Eccolo qui allegato.
Marco E. Ciriotti
«Things are interesting only in so far as they relate themselves to other things»
«Things are interesting only in so far as they relate themselves to other things»
Re: Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet
Molto interessante, grazie Marco.
Michiel Desittere
Benedetti siano gli istanti
e i millimetri
e le ombre delle piccole cose.
(Fernando Pessoa)
Benedetti siano gli istanti
e i millimetri
e le ombre delle piccole cose.
(Fernando Pessoa)
-
- Messaggi: 546
- Iscritto il: sab 27 apr, 2013 13:32
Re: Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet
StudieròMarco E. Ciriotti ha scritto: ↑sab 14 mag, 2022 18:07Sì, certo.
Te lo passo non appena lo avrò dagli autori.
Eccolo qui allegato.
2021_Cesare_et_al_EPSL(1).pdf

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