Dr Kierran Maher

Lecturer in Earth Sciences, School of Environmental and Rural Sciences
Contact
| Email: | kmaher6@une.edu.au |
| Room: | Earth Sciences (C2) Room 211 |
| Phone: | 02 6773 2843 (or +61 2 6773 2843 overseas) |
| Fax: | 02 6773 3300 |
Qualifications
BSc. Engineering Geology, Brigham Young UniversityMS. Geology, Washington State University
Ph.D. Geology, Washington State University
Areas of Teaching
First year geology (GEO110, GEO120 with John Paterson)Ore deposit geology (GEOL207, GEOL305)
Exploration and Environmental geology (GEOL303)
Research Interests
My research interests involve investigating the controls on ore precipitation from hydrothermal fluids and subsequent remobilization. My previous research has involved the use of geochemical and isotopic characteristics to better understand these controls. Specifically, new frontiers in ore deposit research have opened up with the evaluation of transition metal isotopic systems (Cu, Zn, Fe). My present research along these lines is experimentally characterizing mineral-fluid copper isotope fractionation factors for chalcopyrite so that the measured isotopic data from ore deposits can be more clearly interpreted. Of significance is the recognition of measurable copper isotopic variability in high temperature Cu-ore which indicates that high temperature (>250 °C) fluid-mineral isotopic fractionations occur in ore deposits. This fact can be used to better understand transport and deposition mechanisms of the ore metal itself.Other interests I have include the metallogeny of the porphyry-skarn hydrothermal systems of the Andahuaylas-Yauri Batholith of Southeastern Perú. Present research I am undertaking investigates the genesis of massive replacement magnetite bodies, and their relationship to economic mineralization. This requires the utilization of several facets of geochemical analysis, including trace element and isotopic geochemistry of hydrothermal magnetite. As magnetite bodies commonly occur in many porphyry-related skarn systems, several Australian analogues will be compared in this study.
