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Durango M Eacutexico Ore Gold Ore

Jan 01 2001 The La Ci nega gold-silver veins are low-sulfidation epithermal-type deposits related to a rhyolitic flow-dome complex. Ore deposits in the La Ci nega district consist of a series of subparallel northwest– southeast-trending veins which are hosted in andesitic and rhyolitic rocks that belong to the Tertiary-age Upper and Lower Volcanic sequences.

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