PGE-bearing Alaskan-type mafic-ultramafic intrusion.
Located on the west side of the Western Cordillera, in the headwaters area of the Condoto and San Juan rivers.
References:
- Stribrny, B., Wellmer, F.-W., Burgath, K.-P., Oberthür, T., Tarkian, M., and Pfeiffer, T. (2000): Unconventional PGE occurrences and PGE mineralization in the Great Dyke: metallogenic and economic aspects. Mineralium Deposita 35, 260-281.
Mineral List:13 entries listed. 9 valid minerals.
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