Geochemistry Characteristics of Cenozioc Alkaline-Rich Intrusions and its Forming Tectonic Setting in Jiudingshan Porphyry Cu-Mo Polymetallic Deposit, West Yunnan

Yan Dao; Feng Li; Wang Rong

doi:10.4028/www.scientific.net/AMR.868.125

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HomeAdvanced Materials ResearchAdvanced Materials Research Vol. 868Geochemistry Characteristics of Cenozioc...

Geochemistry Characteristics of Cenozioc Alkaline-Rich Intrusions and its Forming Tectonic Setting in Jiudingshan Porphyry Cu-Mo Polymetallic Deposit, West Yunnan

Abstract:

Geochemistry Characteristics of iudingshan Porphyry Cu-Mo Polymetallic Deposit are analyzed in the presented work. The Jiudingshan alkaline-rich porphyry is formed in Cenozoic (from 52 Ma to 29 Ma), being characterized by high potassium, rich alkali and high alumina can be attributed to high K calc alkaline series and shoshonite series, which showing LREE enrichment, HREE depletion, weak negative Eu anomaly (δEu=0.72~1.02, av.=0.86) close to the crust-mantle granite type (δEu=0.83) and mainly is formed in a post-collisional intraplate tectonic setting.

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Periodical:

Advanced Materials Research (Volume 868)

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125-128

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.868.125

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Online since:

December 2013

Authors:

Yan Dao, Feng Li*, Wang Rong

Keywords:

Alkaline-Rich Intrusion, Geochemistry, Jiudingshan, Tectonic Setting

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