MINERALOGY AND CHEMISTRY OF SILICATE MINERALS IN SKARN DEPOSITS ON EXPECTATION MOUNTAIN NEAR RICO, COLORADO: INSIGHT INTO METAMORPHIC HISTORY AND CONTROLS
The Cu-Fe skarns hosted by the Permian Cutler Formation on Expectation Mountain are distinguished by assemblages of garnet + quartz + calcite + epidote-clinozoisite ± actinolite-hornblende ± muscovite ± adularia ± retrograde chlorite. These associations are consistent with a broad peak metamorphic temperature range of 400-600°C in a low pressure environment (estimated at 0.02 GPa). Complex zoning in garnet (82.9% Adr, 15.2% Grs) porphyroblasts reveal fluctuations in composition that were probably influenced by rapid shifts in oxygen fugacity or other environmental conditions. Micron-scale oscillatory zoning and anisotropism highlight the chemical variations between andradite-rich and grossular-rich zones.
The silicate-carbonate assemblages of skarn deposits in the Cutler Formation are broadly similar to those of Pb-Zn-Cu-Ag skarns in the Rico district hosted by carbonate and pelitic strata in the Leadville Limestone and Hermosa Formation. These skarns are distinguished by the presence of carbonates + garnets ± epidote-clinozoisite ± tremolite ± diopside-hedenbergite ± actinolite-hornblende ± chlorite ± albite ± potassium feldspar. Our investigation reveals, however, that the mineral assemblages in high-grade Fe-Cu-Au skarns at Expectation Mountain are more compositionally restricted which is indicative of these deposits. These results are consistent with historical accounts of Fe-Cu-Au skarn deposits in the Cutler Formation in the La Plata Mountains, and other locations in the western San Juan Mountains.