Skip Navigation | ANU Home | Search ANU | Directories
The Australian National University
Research School of Earth Sciences
Printer Friendly Version of this Document
RSES SITE SEARCH
Untitled Document

Dr. Greg Yaxley

Research Fellow

Research School of Earth Sciences
The Australian National University
Canberra 0200
AUSTRALIA

T: +61 2 6125 8334
F: +61 2 6125 4835
E: Greg.Yaxley@anu.edu.au

Biography

Publications

Current Research

Student Projects

PRISE Commercial and Collaborative Activities


  • Major and trace element analysis and interpretation of diamond indicator minerals (garnet, Cr-diopside, Cr-spinel, zircon, perovskite etc).
    More information about our capabilities is available here.
  • Laser Ablation ICPMS - Trace element determinations of geological and other materials using LA-ICPMS.
  • Electronprobe microanalysis - Major and minor element analysis of mineral phases and glass.
  • High pressure experimentation - mineralogical or petrological investigations of high pressure phase relations can be conducted using the range of solid media high pressure apparatuses available at RSES.

Research Interests

  • Development and application of the synchrotron-based techniques XANES for determination of Fe 3+ /?Fe in garnet - application to lithospheric oxygen fugacity and diamond stability.
    Read more here.
  • Melting of heterogeneous mantle - Compositional heterogeneities are introduced into the convecting mantle by recycling of mafic materials at convergent margins. Based on geochemical and fluid dynamic evidence they may have a role in petrogenesis of many lavas including MORBs, OIBs and flood basalts. But how does such heterogeneous mantle actually melt, and what is the nature of the liquids produced?
  • Melt inclusions in primitive lavas - Tiny samples of melt trapped in phenocrysts in primitive magmas may be near primary melts, providing important information about mantle melting and magma sources. It is also possible that they reflect shallower processes occuring in the plumbing systems of some magma systems. Our recent investigations suggest the latter is important in the case of the Baffin Island picrites.
  • Petrogenesis of carbonatites and kimberlites