Abstract
The San Francisco gold deposit is located 145 km north of Hermosillo, Sonora. Its geology includes a Precambrian metamorphic-igneous complex, a Jurassic meta-volcanosedimentary sequence and small bodies of Tertiary intrusions. The mineralization is hosted in a leucocratic deformed granite affected by Tertiary hydrothermal alteration… in order to continue, download the full paper in PDF.
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