URI | http://purl.tuc.gr/dl/dias/5AE54AF3-4930-460D-BBB0-BD992A0FDE6E | - |
Αναγνωριστικό | https://doi.org/10.2138/am.2008.2662 | - |
Γλώσσα | en | - |
Μέγεθος | 8 pages | en |
Τίτλος | White mica domain formation: A model for paragonite, margarite, and muscovite formation during prograde metamorphism | en |
Δημιουργός | Christidis Georgios | en |
Δημιουργός | Χρηστιδης Γεωργιος | el |
Δημιουργός | Kenneth J. T. Livi | en |
Δημιουργός | Péter Árkai | en |
Δημιουργός | David R Veblen | en |
Περίληψη | Scanning transmission electron microscopy images of the 00l white mica planes in crystals from
central Switzerland and Crete, Greece, reveal that domains of paragonite, margarite, and muscovite
are ordered within the basal plane. Energy dispersive X-ray analyses show that both cations in the
interlayer and in the 2:1 layer have ordered on the scale of tens to hundreds of nanometers. Domain
boundaries can be both sharp and crystallographically controlled or diffuse and irregular. A model
outlining the domain formation process is presented that is consistent with X-ray powder diffraction
and transmission electron microscopy data. The domain model incorporates aspects of a mixedlayered
and a disordered compositionally intermediate phase models. The main feature of the model
is the formation of mica species that segregate within the basal plane and contradict the notion of
homogeneous layers within mixed-layer phases. Implications for the formation of all diagenetic and
very low-grade metamorphic 2:1 sheet silicates are discussed | en |
Τύπος | Peer-Reviewed Journal Publication | en |
Τύπος | Δημοσίευση σε Περιοδικό με Κριτές | el |
Άδεια Χρήσης | http://creativecommons.org/licenses/by/4.0/ | en |
Ημερομηνία | 2015-10-01 | - |
Ημερομηνία Δημοσίευσης | 2008 | - |
Βιβλιογραφική Αναφορά | J. T. Kenneth Livi ,G.E. Christidis ,Péter Árkai ,D. R Veblen , " White mica domain formation: A model for paragonite, margarite, and muscovite formation during prograde metamorphism ",Am. Mineral. ,vol. 93,no.4 pp.520-527 ,2008.doi :10.2138/am.2008.2662 | en |