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| Description | |
|---|---|
| Comments: | Most abundant sulfide mineral. |
| Quality of samples: | not specified / average specimens |
| Confirmation | |
| Validity: | Believed Valid |
| References | |
| References: | Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 132, 341; Schwartz, G.M. (1947), Hydrothermal alteration in the 'porphyry copper' deposits, Econ.Geol.: 42: 319-352; Schwartz, G.M. (1949), Oxidation and enrichment in the San Manuel copper deposit, AZ, Econ.geol.: 44: 253-277; Schwartz, G.M. (1958), Alteration of biotite under mesothermal conditions, Econ.Geol.: 53: 164-177; Lovering, T.S. (1948), Geothermal gradients, recent climate changes, and rate of sulphide oxidation in the San Manuel district, AZ, Econ.Geol.: 43: 1-20; Creasey, S.C, (1959), Some phase relations in the hydrothermally altered rocks of porphyry copper deposits, Econ.Geol.: 54: 351-373; . |
| Associated minerals: | |
| Associates: | Chalcopyrite Endellite Quartz Sericite |
| Data | |
| Mineral Data: | Click here to view Pyrite data |
| Locality Data: | Click here to view San Manuel orebody, San Manuel Mine (Apex Lead & Vanadium Mining Corp Mine; Quarelli group), San Manuel, San Manuel District, Pinal Co., Arizona, USA |
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