Sign Up to like & get
recommendations!
0
Published in 2019 at "Contributions to Mineralogy and Petrology"
DOI: 10.1007/s00410-019-1607-1
Abstract: Because of the strong preference of fluorine (F) for “hydrous” magnesian silicate minerals, the temperature T(0F) given by the reaction (Bi–Gt) of Fe–Mg exchange between biotite and garnet [phlogopite (Phl) + almandine (Alm) = annite (Ann) + pyrope (Py)] can be…
read more here.
Keywords:
effect;
biotite garnet;
fluorine;
thermometry ... See more keywords