DECODING THE RHYTHMS OF PORPHYRY COPPER SYSTEMS (Invited Presentation)
Through integrating deposit geology, fluid inclusion microthermometry, high-precision Re-Os molybdenite dating and oxygen isotope analysis of quartz-molybdenite veins from the Qulong system, we show that fluid evolution under an absolute timeframe was cyclic. We further demonstrate that such a process can be decoded from high spatial resolution oxygen isotopic analysis in a relative timeframe fashion. Specifically, our SIMS oxygen isotope data of single-grain hydrothermal quartz from the Qulong porphyry copper system faithfully record meteoric water incursion during episodic fluxing of magmatic fluids.
In line with multiple generations of intrusions and recent advances in high resolution chronological/isotopic analysis and numerical modelling, we suggest that cyclicity is an ubiquitous feature for ore formation that ultimately linked to dynamic evolution of underlying magmatic reservoirs.
Key References
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3 Li, Y., Selby, D., Condon, D. & Tapster, S. Cyclic Magmatic-Hydrothermal Evolution in Porphyry Systems: High-Precision U-Pb and Re-Os Geochronology Constraints on the Tibetan Qulong Porphyry Cu-Mo Deposit. Economic Geology 112, 1419-1440 (2017).
4 Chelle-Michou, C., Rottier, B., Caricchi, L. & Simpson, G. Tempo of magma degassing and the genesis of porphyry copper deposits. Scientific Reports 7, 40566 (2017).