-
Forsterite (Mg2SiO4;
commonly abbreviated as Fo; also
known as
white olivine) is the magnesium-rich end-member of the
olivine solid solution series. It...
- will
cause both
windows to
appear the same
color (violet).
Synthetic forsterite (Mg2SiO4, the magnesium-rich end-member of olivine) has also been sold...
- as
molar percentages of
forsterite (Fo) and/or
fayalite (Fa) (e.g., Fo70Fa30, or just Fo70 with Fa30 implied).
Forsterite's melting temperature is unusually...
-
Fayalite forms solid solution series with the
magnesium olivine endmember forsterite (Mg2SiO4) and also with the
manganese rich
olivine endmember tephroite...
- is
complete at
about 750 °C (1,380 °F), with the
final products being forsterite (magnesium silicate),
silica and water. The
global m****
balance reaction...
-
indicate that tiny
forsterite crystals might be
falling down like rain on to the
protostar HOPS-68. The
discovery of the
forsterite crystals in the outer...
-
contain iron and hydrogen. It is
polymorphous with the
olivine phase forsterite (a
magnesium iron silicate).
Ringwoodite is
notable for
being able to...
- two or more
endmembers in a
group or
series of minerals. For example,
forsterite (Mg 2SiO 4) and
fayalite (Fe 2SiO 4) are the two end-members of the olivine...
- tremolite, talc, and
forsterite for the albite-epidote
hornfels facies; calcite, dolomite, quartz, tremolite, diopside, and
forsterite for the hornblende...
-
dominated by iron-poor
pyroxene and olivine, as
represented by
enstatite and
forsterite, respectively,
along with sodium-rich
plagioclase and
minerals of mixed...
