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Cordilleran Vein Type Deposits Examples

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<strong>Vein</strong>s 11/3/10<br />

Generaliza>ons -­‐1<br />

• Associa>on in space and >me with calc-­‐<br />

alkaline igneous ac>vity<br />

• Hydrothermal transport of ore components,<br />

deposited epigene>cally in faults<br />

• Ore minerals as typical open-­‐space fillings<br />

or co-­‐precipitates in silicate host rocks and<br />

as replacements in carbonate hosts<br />

• Deposi>on within 1+ km of the surface<br />

• Well developed metal zona>on<br />

Generaliza>ons-­‐2<br />

• Sulfur isotope ra>os close to 0 ‰<br />

• Structural control<br />

• Typically well-­‐developed bilaterally<br />

symmetrical wall-­‐rock altera>on<br />

• Normally contain porphyry-­‐Cu suite of<br />

elements with zona>on from (Sn-­‐W-­‐)Mo-­‐<br />

Cu-­‐Zn-­‐Pb-­‐Mn-­‐Ag<br />

• Magma>c-­‐hydrothermal fluids mixed (late,<br />

post-­‐ore?) with meteoric fluids<br />

2

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