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2009-04-20_GENERAL DOCUMENTS - M2009076 (6)
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2009-04-20_GENERAL DOCUMENTS - M2009076 (6)
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8/24/2016 3:45:43 PM
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DRMS Permit Index
Permit No
M2009076
IBM Index Class Name
GENERAL DOCUMENTS
Doc Date
4/20/2009
Doc Name
Declaratory Order Presentation- Part 1
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Venture Resources
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DRMS
Permit Index Doc Type
Gen. Correspondence
Media Type
D
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In contrast to neighboring areas, granitic rocks are sparse in the Idaho Springs district. The few bodies <br />• of granitic rocks large enough to show on plate 2 are small and appear to be satellite to the larger plutons or <br />batholiths that crop out to the southwest, west, and north of the district. The granodiorite is similar to the <br />Boulder Creek Granite (Lovering and Goddard, 1950, p. 25-27) ; the biotite-muscovite granite is similar to the <br />Silver Plume Granite from the type locality at Silver Plume, Colo., about 16 miles southwest of Idaho Springs <br />(Ball, 1906). Lithologic names rather than geographic formational names are used here because the stratigraphy <br />of the Precambrian metasedimentary rocks and correlations of the intrusive rocks are not fully established. <br />GNEISSIC ROCKS <br />The gneissic rocks are divided into three major lithologic units: microcline gneiss (or microcline- <br />quartz-plagioclase-biotite gneiss), biotite gneiss (or interelayered biotite gneisses) , and granite gneiss (or <br />granite gneiss and pegmatite). The biotite gneiss and granite gneiss are grouped on plate 2, and together they <br />are conformably interlayered with units of microcline gneiss. If these units are assumed not to be overturned, a <br />stratigraphic succession can be recognized as shown in section B-B' of plate 2. The lowermost unit, a thick <br />layer of mixed biotite gneiss and granite gneiss, forms the core of the Idaho Springs anticline on the southeast <br />side of the district. This lowermost unit is overlain by a thin and discontinuous layer of microcline gneiss. The <br />microcline gneiss, in turn, is overlain by a thick layer of mixed biotite gneiss and granite gneiss. A thick unit of <br />microcline gneiss is higher in the stratigraphic succession, and it is overlain by a thick layer of mixed biotite <br />gneiss and granite gneiss - the uppermost unit in the district. <br />In addition to these major units, small bodies of amphibolite, calc-silicate gneiss, and quartz gneiss are <br />exposed, but these small outcrops are not shown on plate 2. All the gneissic rocks are described here without <br />regard to their apparent stratigraphic position. <br />• BIOTITE GNEISS <br />Two main varieties of biotite gneiss are recognized: biotite-quartz-plagioclase gneiss and sillimanitic <br />biotite-quartz-gneiss, both of which are locally garnetiferous. These rocks alternate with one another in layers <br />that range from about an inch to several feet in thickness and probably represent the original bedding. In <br />outcrops the biotite gneiss is marked by its dark-gray color, pronounced layering, and tendency to split parallel <br />to the layering. Conformable layers and lenses of granite gneiss, present in most exposures, emphasize the <br />layered appearance of the unit. <br />Typical biotite-quartz-plagioclase gneiss is fine grained, equigranular, light to dark gray, and is faintly <br />to intensely foliated. The gneiss typically contains quartz and plagioclase in nearly equal amounts and 19-35 <br />percent biotite. The feldspar composition generally ranges from oligoclase to andesine. Foliation is produced by <br />a parallel alignment of biotite and locally by segregation of minerals into light and dark layers. <br />The sillimanitic biotite-quartz gneiss is light to dark gray and is well foliated; it is flecked with pock <br />and smears of white fibrous sillimanite and. has a marked schistose structure. The rock contains abundant <br />quartz, about 20 percent biotite, as much as 30 percent sillimanite (but generally much less), and, commonly, <br />some microcline and albite-oligoclase. Small amounts of muscovite can be found in most specimens, and garnet <br />(almandine-spessartite) is locally abundant. <br />GRANITE GNEISS AXD PEGMATITE <br />Granite gneiss (or granite gneiss and pegmatite) is exposed throughout the district in layers and lenses <br />that range in thickness from less than an inch to several hundred feet. It is generally associated with biotite <br />gneiss, and in many places relatively equal amounts of these two rock types are intimately mixed in thin <br />alternating layers that form migmatite. Granite gneiss, some of which is also associated with microcline gneiss, <br />is most abundant, in the southwest corner of the district. Northeastward, layers of biotite gneiss are more <br />• abundant, and layers of granite gneiss are less abundant and discontinuous. <br />6
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