Abstract
The Cameca IMS 3f ion microprobe at Arizona State University has been modified to allow the analysis of 18O/16O ratios on 10- to 20-micrometer spots in insulating minerals in thin section. A primary beam of K+ or Cs+ is used, and charge is neutralized by an electron flood gun operating at -7.5 kilovolts. Negative secondary ions are accelerated to -4.5 kiloelectronvolts into the mass spectrometer, where 18O- is detected on the electron multiplier by pulse counting, and 16O- is detected on the electron multiplier or directly measured by an electrometer. In either configuration, internal precisions of 1.2 to 1.7 per mil (1 standard error of the mean) in 18O/16O ratios can be achieved. Preliminary analyses, showing quartz to be 10 to 15 per mil lighter than hydrothermally altered plagioclase, suggest that matrix effects are important. -Authors
Original language | English (US) |
---|---|
Pages (from-to) | 137-143 |
Number of pages | 7 |
Journal | US Geological Survey Bulletin |
Volume | 1890 |
State | Published - 1989 |
ASJC Scopus subject areas
- Geology