Synthetic high-pressure micas compositionally intermediate between the dioctahedral and trioctahedral mica series

T. H. Green*

*Corresponding author for this work

Research output: Contribution to journalArticle

8 Citations (Scopus)

Abstract

Intermediate-composition micas with octahedral occupancy ≳2.5 have been crystallized experimentally from natural phengite, 50% phengite+50% biotite, and synthetic basalt compositions in the pressure range 20-35 kb and temperatures of 800-1,000° C. Their compositions suggest a complete range of micas with octahedral occupancy between 3.0 and 2.5, but a very restricted range between 2.0 and 2.5. These 2.5-octahedral micas lie close to the new mica series proposed by Seifert and Schreyer (1965, 1971), with one end-member composition of K Mg2.5 (Si4O10) (OH2) which is extended by the present results into alumina-bearing members of the series (e. g. K Mg1.5 Al1.0 (Si3Al1.0O10) (OH)2). However, the possibility of interlayering of dioctahedral and trioctahedral micas to give an apparently intermediate composition cannot be ruled out. X-ray powder diffraction data on the critical 060 reflection for the phengite mix suggest a transitional change from a single phengite field, through a 2-phase phengite - 2.5-octahedral mica field to a single phase 2.5-octahedral mica field. Natural micas of similar composition have not so far been identified, due probably to the unlikelihood of obtaining a mineralogical record of an appropriate composition at the restricted pressure and temperature conditions apparently needed to stabilize the 2.5-octahedral mica phase. Nevertheless, such a phase may have an important role in mineral assemblages and melting reactions in the deep continental crust, subducted oceanic crust and in the upper mantle; evidence of its existence may be removed by later, lower-pressure reactions.

Original languageEnglish
Pages (from-to)452-458
Number of pages7
JournalContributions to Mineralogy and Petrology
Volume78
Issue number4
DOIs
Publication statusPublished - Mar 1982

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