An overview of vis-nir-swir field spectroscopy - Spectral International
An overview of vis-nir-swir field spectroscopy - Spectral International
An overview of vis-nir-swir field spectroscopy - Spectral International
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Figure 60 - Actinolite, tremolite, epidote,<br />
clinozoisite, Fe-Chlorite, Mg-chlorite,<br />
biotite, phlogopite, vesuvianite, and<br />
prehnite<br />
47<br />
Figure 61 - Forsterite, serpentine, talc, calcite,<br />
tremolite, and magnetite<br />
MAGNESIUM SKARN<br />
Magnesium skarns are developed as<br />
metasomatic replacements <strong>of</strong> dolomitic<br />
limestone. High temperature magnesium<br />
skarns are characterized by forsterite, and<br />
diopside and low temperature magnesium<br />
skarns contain serpentine and talc. Both <strong>of</strong><br />
which occur as retrograde minerals after<br />
forsterite and clinopyroxene.<br />
Figure 61 plots forsterite, serpentine, talc,<br />
calcite, tremolite, magnetite.
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