2011Acta Geoscientica SinicaRequires access

The Petrogenic age of Narigongma Granitic Diorite-porphyry in the Northern Part of the Sanjiang Region and Its Geological Implications

LI Ya-zhi

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Abstract

The Narigongma porphery molybdenite copper deposit related to intrusive rocks was discovered recently in the northern part of the Sanjiang Region.U-Pb dating shows that the formation age of Narigongma granodiorite porphyry is 41.44±0.23 Ma,belonging to early Himalayan period.Metallogenic ages of the Narigongma porphery molybdenite copper deposit are mainly in the range of 40.8±0.4 Ma~40.86±0.85 Ma.During multiperiodic hydrothermal activities and multistage ore-forming processes,the metallogenetic hydrothermal solution was provided by Narigongma granitite porphyry(41.53±0.24 Ma),Narigongma granite diorite-porphyry(41.44±0.23 Ma) and Narigongma plagioclase porphyry(41.00±0.18 Ma).Due to occurrence of many intermediate-acid mass,the age of these intrusive bodies provide evidence for collision function between India plate and Eurasian plate in 65~45 Ma,which has theoretical and practical meaning to forecast of porphyry copper-molybdenum deposit in the region.

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What this paper is about

The Narigongma porphery molybdenite copper deposit related to intrusive rocks was discovered recently in the northern part of the Sanjiang Region.U-Pb dating shows that the formation age of Narigongma granodiorite porphyry is 41.44±0.23 Ma,belonging to early Himalayan period.Metallogenic ages of the Narigongma porphery molybdenite copper deposit are mainly in the range of 40.8±0.4 Ma~40.86±0.85 Ma.During multiperiodic hydrothermal activities and multistage ore-forming processes,the metallogenetic hydrothermal solution was provided by Narigongma granitite porphyry(41.53±0.24 Ma),Narigongma granite diorite-porphyry(41.44±0.23 Ma) and Narigongma plagioclase porphyry(41.00±0.18 Ma).Due to occurrence of many intermediate-acid mass,the age of these intrusive bodies provide evidence for collision function between India plate and Eurasian plate in 65~45 Ma,which has theoretical and practical meaning to forecast of porphyry copper-molybdenum deposit in the region.

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Available abstract

The Narigongma porphery molybdenite copper deposit related to intrusive rocks was discovered recently in the northern part of the Sanjiang Region.U-Pb dating shows that the formation age of Narigongma granodiorite porphyry is 41.44±0.23 Ma,belonging to early Himalayan period.Metallogenic ages of the Narigongma porphery molybdenite copper deposit are mainly in the range of 40.8±0.4 Ma~40.86±0.85 Ma.During multiperiodic hydrothermal activities and multistage ore-forming processes,the metallogenetic hydrothermal solution was provided by Narigongma granitite porphyry(41.53±0.24 Ma),Narigongma granite diorite-porphyry(41.44±0.23 Ma) and Narigongma plagioclase porphyry(41.00±0.18 Ma).Due to occurrence of many intermediate-acid mass,the age of these intrusive bodies provide evidence for collision function between India plate and Eurasian plate in 65~45 Ma,which has theoretical and practical meaning to forecast of porphyry copper-molybdenum deposit in the region.

Key concepts: Molybdenite, Diorite, Geology, Geochemistry, Porphyry copper deposit, Hydrothermal circulation, Plagioclase, Seismology

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