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MINEBK00806
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Last modified
1/9/2009 1:08:41 PM
Creation date
11/18/2007 12:18:21 PM
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Mine Books
County
Pitkin
Volume
8
Document
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A
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GEOLOGY. , <br />3 <br />}sere is n good geological survey of the district made by Spurr of the <br />i <br />U.S.C.S. <br />Tho ore bodies occur in the'Cnrhninferoun~fnrrmtinn principally in the <br />contact bstt:eon the hro:vn line nr Lendville dolor.3lteCctndathefb>bue}lime. <br />The are tfodies of the Durant-Anpenr&.nre found on the east limb of the <br />;Aspen Lit.synclinerwhich becor.~e.^. very steep n little below surfacerturn- <br />ling dovrn so as to become vertical rand even overturning locally ao as <br />to dip to the eant.After t$is steepening the beds recover and assume a <br />iflattor dip to the rreat.Iiear change of dip the Aspen fault in developed <br />vertical vrith a alight throw. Piest of the ltnpen fault another fault be- <br />',longing to name systera in developed called the Schiller, <br />:The ore in c}:iefly found in .a narrow vertical zone batvreon the aspen and <br />', Contact fnultn..blany other minor faults }wove. been developed which also <br />!~}tave afforded favorable placer for the deposition of large pro bodies . <br />The ore is nearly always found in t}:n dolomite nt the intersection of <br />one or more of these fnultn vrith tar Contact fault. r <br />T}te ore.n in' the Durant varyrhotF, in coraponitiott and quality. A large <br />amount of oxidized arc. has been taY.en out from cror}an,;s near surface, <br />the srtme changing to sulp}:ides •rrith dept}t,though Home oxidized ores <br />are to be found in ]saver eror}:in};n, i7te ore is chiefly an argentiferous <br />I galonarwhich har, re}ilnced tho dolomite and limestone to a greater or <br />I <br />j less extent. In some of the ores the silver occurs in the form of <br />arKehtite ar nulpi'.idc. There in also considerable sulp}tide and car- <br />~ borate of zinc. <br />TA.e Schiller workings lie vrest of the Durant and consequently the <br />ore horizon is lntver dovrn. <br />The A.J.workingn are a] no run on th (:orttact fault betwer+rt the dolomite <br />and blue limerporphyry and shale are to be seen same being due to <br />crown faulting. <br />~ GoinF; crust on Aspen bit. we find the Sara Jane and, Saddle Pock faults <br />along whic~re is-found and being on the went limb of the Aapen'Lit. <br />synoline. An intrusive porphyryrcoc~anly known an quartz porphyry i2 <br />
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