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Geology; July 2008; v. 36; no. 7; p. 547-550; DOI: 10.1130/G24580A.1
© 2008 Geological Society of America
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Trace elements in hydrothermal quartz: Relationships to cathodoluminescent textures and insights into vein formation

Brian G. Rusk1,*, Heather A. Lowers1 and Mark H. Reed2

1 U.S. Geological Survey, MS 973, Denver, Colorado 80225, USA
2 Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA

High-resolution electron microprobe maps show the distribution of Ti, Al, Ca, K, and Fe among quartz growth zones revealed by scanning electron microscope-cathodoluminescence (SEM-CL) from 12 hydrothermal ore deposits formed between ~100 and ~750 °C. The maps clearly show the relationships between trace elements and CL intensity in quartz. Among all samples, no single trace element consistently correlates with variations in CL intensity. However in vein quartz from five porphyry-Cu (Mo-Au) deposits, CL intensity always correlates positively with Ti concentrations, suggesting that Ti is a CL activator in quartz formed at >400 °C. Ti concentrations in most rutile-bearing vein quartz from porphyry copper deposits indicate reasonable formation temperatures of <750 °C using the TitaniQ geothermometer. Titanium concentrations of <10 ppm in all veins that formed at temperatures <350 °C suggest a broad correlation between Ti concentrations and temperature of quartz precipitation.

In quartz from most deposits formed at <350 °C, bimodal Al concentrations exist wherein some growth bands contain <50 ppm and others contain >2000 ppm, but in high-temperature quartz, Al concentrations are consistently in the range of several hundred ppm. Aluminum concentrations in quartz reflect the Al solubility in hydrothermal fluids, which is strongly dependent on pH. Aluminum concentrations in quartz therefore reflect fluctuations in pH that may drive metal-sulfide precipitation in hydrothermal systems.

Key Words: quartz • vein • cathodoluminescence • trace elements • hydrothermal • microprobe






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