Epidote minerals are known since the 18th century, but at that time the greenish to dark
colored varieties were termed actinolite or schorl and not distinguished from the minerals to …

The thermodynamic properties of 254 end‐members, including 210 mineral end‐members,
18 silicate liquid end‐members and 26 aqueous fluid species are presented in a revised …

The thermodynamic properties of 154 mineral end‐members, 13 silicate liquid end‐
members and 22 aqueous fluid species are presented in a revised and updated data set …

A correlation of OH stretching frequencies (from infrared spectroscopy) with O… O and H…
O bond lengths (from structural data) of minerals was established. References on 65 …

Numerous spectroscopic techniques have been applied to the epidote minerals to
characterize their structure and crystal chemistry. The substitution of transition metal ions …

The fluid-absent reaction 12 zoisite= 3 lawsonite+ 7 grossular+ 8 kyanite+ 1 coesite was
experimentally reversed in the model system CaO-Al 2 O 3-SiO 2-H 2 O (CASH) using a …

Substantially identical Mössbauer spectra (Fig. 1) have been collected at room temperature
from the type sample (TsH–9026) and a second one (TsH–9031) with an absorber thickness …

The lattice parameters of kyanite were measured at various pressures up to about 60 kbar
by single-crystal X-ray diffraction in a diamond anvil cell. Unit-cell dimensions decreased …

Heflikite, the first Sc-dominant epidote-supergroup mineral, was discovered in two
occurrences. The holotype was found in a granitic pegmatite associated with rodingite-like …

The single-crystal elastic constants of zoisite Ca2Al3Si3O12 (OH) were determined by
Brillouin scattering at ambient conditions. The elastic tensor was obtained by an inversion of …