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Title: Altered igneous rocks around Rocky Mountain manto deposits: the Gilman (Colorado) example

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6196534

The Pando Porphyry at Gilman, Colorado forms an easterly-dipping sill above a major manto sulfide ore deposit hosted in the Leadville Dolomite. The sill is regionally altered to a propylitic assemblage (chl-epid-carb). Above the ore bodies the base of the sill is regionally altered to a phyllic assemblage (2M mica-qtz-py-kaol). The phyllic zone is divisible using birefringence of 2M mica into three subzones, which are mineralogically identical and gradational into one another. The phyllic zone is surrounded by a kaolinite-rich argillic zone with local sparse smectite. Spatially, the phyllic alteration is closely confined to the area of the ore bodies. Moreover, the thickness of phyllically altered porphyry is directly correlated with the intensity of mineralization. The distribution of alteration in the Pando sill (age = 70 Ma) requires that the manto mineralization process was at least predominantly: 1) hydrothermal; 2) Tertiary in age; and 3) had up-dip hydrothermal flux along the base of the sill. The sequence propyllitic-argillic-phyllic-ore is present at several other large Rocky Mountain manto deposits and argues for an epigenetic origin involving high-T, low-pH fluids.

Research Organization:
Camino Viviente, Goleta, CA (USA)
OSTI ID:
6196534
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English