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PACRIM has turn into the leading AusIMM geological convention at the Pacific Rim, bringing jointly the latest advances in primary educational learn, local surveys through govt businesses and the industry’s most modern discoveries to exhibit the significance of the Pacific Rim for international mineral wealth. This 2008 quantity will entice any geologist, geophysicist, or geochemist exploring within the Pacific Rim or drawn to mineralization approaches in energetic tectonic margins. The lawsuits disguise the components of the West Pacific and South-East Asia, the Andean area and relevant the US, featuring the state of the art in ore deposits examine in those areas.
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GNS Science, PO Box 30368, Lower Hutt 5040, New Zealand. 5. University of Kyushu, Fukuoka 812-8581, Japan. 6. Woods Hole Oceanographic Institution (WHOI), 266 Woods Hole Road, Woods Hole MA 02543. 7. University of Kiel, Kiel 24118, Germany. 8. National Institute of Water and Atmospheric Research (NIWA), Private Bag 14901, Wellington, New Zealand. 9. University of Ottawa, Ottawa ON K1N 6N5, Canada. 10. Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka Kanagawa 237-0061, Japan.
Due to the complex basement geology and host rocks, the interpretation of geochemical composition is not trivial and requires consideration of petrography and geological environment of the analysed igneous rocks. THE MAGMATIC AND METALLOGENETIC EVOLUTION All Tertiary igneous rocks were emplaced in a high-K calc-alkaline arc environment. Eocene intrusions and domes are widespread and include dacitic domes west of Cerro de Pasco and several dioritic to rhyolitic intrusions generally emplaced ca 20 km E of the Cordillera Occidental.
42 24 - 26 November 2008 PACRIM Congress 2008 Petrogenetic Relationships and Metallogeny Above Flat Subduction – The Example from Central Peru T Bissig1 and R M Tosdal2 ABSTRACT Intrusion related ore deposits are widespread in the Central Peruvian Cordillera Occidental and adjacent high-plains to the east and include porphyry Cu (-Au, Mo; eg Morococha), Cu-Zn (Pb-) skarn (eg Antamina), Pb-Zn-Ag carbonate hosted vein deposits (eg Uchucchacua), cordilleran base metal (eg Cerro de Pasco) and epithermal deposits (eg Quicay).