Trace-element geochemistry of diamond-hosted olivine inclusions from the Akwatia Mine, West African Craton: implications for diamond paragenesis and geothermobarometry (2019)
Attributed to:
Ion Micro-Probe Facility (IMF)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1007/s00410-019-1634-y
Publication URI: http://dx.doi.org/10.1007/s00410-019-1634-y
Type: Journal Article/Review
Parent Publication: Contributions to Mineralogy and Petrology
Issue: 12