The peculiar crystal-chemistry of phlogopite from metasomatized peridotites: evidence from laboratory and nature

Abstract

Periodico di Mineralogia (2011), 80, 1 (Special Issue), 181-197 - DOI: 10.2451/2011PM0015 Special Issue in memory of Sergio Lucchesi The peculiar crystal-chemistry of phlogopite from metasomatized peridotites: evidence from laboratory and nature Paola Comodi 1,* , Sabrina Nazzareni 1 , Patrizia Fumagalli 2 and Gian Carlo Capitani 3 1 Dipartimento di Scienze della Terra, Universita di Perugia, Italy 2 Dipartimento di Scienze della Terra, Universita di Milano, Italy 3 Dipartimento di Scienze Geologiche e Geotecnologie, Universita di Milano Bicocca, Italy *Corresponding author: comodip@unipg.it Abstract Experimental petrology suggested that phlogopite has a peculiar mineral chemistry at high pressure: excess of Si coupled with a decrease in IV Al and deficiency in K+Na. This K-edenite exchange, □ XII Si(K+Na) -1 Al -1 , where □ XII is a vacancy in the interlayer, should imply that phlogopites incorporate significant amount of talc component. At high pressure conditions, however, in a fluid saturated system, a talc component might translate into a 10 A phase component, being the latter phase the product of the reaction talc + H 2 O = 10 A phase occurring at P = 4 - 5 GPa and at T = 600-700 °C. We aim to study the structure of natural and synthetic phlogopites showing this peculiar mineral chemistry. Samples were analysed by single-crystal X-ray diffraction, powder X-ray diffraction with full profile fitting, EMP, SIMS, TEM and Mossbauer spectroscopy. The natural samples were recovered from spinel and garnet wedge peridotites of the Ulten Zone Eastern Italian Alps, (Italy), whereas synthetic ones were obtained from high pressure synthesis in a K-doped lherzolite system. The single crystal X-ray refinements of natural phlogopites, together with the EMP analysis, showed two coupled substitutions: Tschermak (Si + Mg = IV Al + VI Al) and talc exchanges (□ + Si = K + Al), with no octahedral vacancies. The Rietveld refinement of the synthetic samples confirmed the ipersilicic character and K deficiency found with EMPA and SIMS analysis. The c lattice parameter of both synthetic and natural phlogopites positively correlates with the increase of vacancies at the interlayer site, pointing toward the c lattice parameter of the 10A phase. The tetrahedral α rotation angle of natural phlogopites was about 9°, lower than that expected by Tscherma substitution. The present data indicate that the 10 A phase component, instead of the talc component, stabilizes the phlogopite structure by reducing the α rotation under high pressure condition. This increases the pressure conditions needed to reach the upper limit value for the tetrahedral rotation. Key words : phlogopite; 10 A phase; single crystal X-ray refinements; EMPA; SIMS.