YAO Zhongyou, CUI Jurong, WEI Wenjun, DONG Yanpu, LIU Jun'an. 2017: Geological characteristics and metallogenic stages of the Pongo iron polymetallic ore deposit in Peru. Geological Bulletin of China, 36(12): 2213-2220.
    Citation: YAO Zhongyou, CUI Jurong, WEI Wenjun, DONG Yanpu, LIU Jun'an. 2017: Geological characteristics and metallogenic stages of the Pongo iron polymetallic ore deposit in Peru. Geological Bulletin of China, 36(12): 2213-2220.

    Geological characteristics and metallogenic stages of the Pongo iron polymetallic ore deposit in Peru

    • From Lima, the capital of Peru, to Chala City, there is a 400km long mineralization zone along the Pacific coast. In this zone, there are a number of iron, copper, gold deposits. The copper-gold deposits possess the special IOCG type characteristics, whereas the iron deposits are mainly of skarn type. Pongo is a huge iron deposit. The deposit is located in the Western Cordillera near the western edge of the depression of ICA to Nascar. The deposit is accompanied by copper-gold mineralization. This deposit not only has skarn specialty but also has IOCG features. The authors summarized the geological factors of the deposit and indicated an excellent copper-gold potential. It is also pointed out that the main iron mineralization and the gold-copper sulfides are different in stage and space.
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