Significance of Plutons, Question regarding Plutons |
Significance of Plutons, Question regarding Plutons |
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#1
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![]() Diggin' In! ![]() ![]() Group: Members Posts: 19 Joined: 31-March 16 From: Pensacola, Fl. Member No.: 122,605 ![]() |
I read the thread on the significance of faults. It brought to mind another geology question. I have been doing some reading on the Pikes Peak Batholith and found that the formations of Plutons in this area seem to have a correlation with mineral formation. Can someone expand on this for me please?
-------------------- "I don't want excuses, I want results." Lifelong quote from my father.
Shawnee Man |
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#2
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![]() Rock Bar! ![]() ![]() ![]() ![]() Group: Members Posts: 875 Joined: 25-July 14 From: Westminster, CO Member No.: 117,949 ![]() |
Assuming this guy is who he says he is, it gives a little background on the Cripple Creek district. Taken from here:
QUOTE After Carlin and Homestake, Cripple Creek is the third most productive gold district in the US. The ores from Cripple Creek have an origin different from other gold deposits in the Front Range. The gold at Cripple Creek was formed within or at the margin of a Tertiary volcanic breccia. These rocks occupy a steep-walled volcanic caldera about 4 miles long and 2 miles wide that was a result of gaseous eruptions. Explosive fracturing and subsidence produced shear zones in the breccia and adjacent Precambrian rocks. Along these shear zones, various dikes and irregular masses of volcanic rocks were emplaced, including latite, syenite, phonolite and lamprophyre. These dikes were more porous to fluids than the surrounding Precambrian granitic rocks, and in many places became the conduits for the ore bearing brines. These ore deposits are epithermal and found along persistent veins. Many of these veins lie close to the margin of the breccia mass while others persist into the breccia or extend into the adjacent Precambrian rocks. The veins are narrow, high-grade zones mineralized with gold, silver and copper tellurides, pyrite, sphalerite, galena and tetrahedrite. The gangue minerals (associated minerals with no value) are chiefly quartz and fluorspar, with dolomite, ankerite and celestite. The most spectacular discovery at Cripple Creek was the Cresson Vug. This cavity, roughly 25 feet by 12 feet by 40 feet high, was found in 1914, and was lined with gold tellurides, quartz, celestite and clay. Nearly 20,000 ounces of gold had been mined from this vug. -------------------- Lifetime Member
opera non verba "All courses of action are risky, so prudence is not in avoiding danger (it's impossible), but calculating risk and acting decisively. Make mistakes of ambition and not mistakes of sloth. Develop the strength to do bold things, not the strength to suffer." ~Niccolò Machiavelli Ref Code: EM448 |
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#3
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![]() Diggin' In! ![]() ![]() Group: Members Posts: 19 Joined: 31-March 16 From: Pensacola, Fl. Member No.: 122,605 ![]() |
Assuming this guy is who he says he is, it gives a little background on the Cripple Creek district. Taken from here: Thank you Emac. That certainly addressed my request. I find the formation of intrusions fascinating.
-------------------- "I don't want excuses, I want results." Lifelong quote from my father.
Shawnee Man |
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#4
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Diggin' In! ![]() ![]() Group: Members Posts: 16 Joined: 29-March 16 Member No.: 122,603 ![]() |
Thank you Emac. That certainly addressed my request. I find the formation of intrusions fascinating. I like this stuff also, I like to know all the how and why behind all these minerals etc. Hopefully makes me a better rockhound than just going to the locations everyone knows about. |
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