|August 2016 - Present||Assistant Professor, Geology and Geophysics, Missouri University of Science and Technology ‐ Geosciences and Geological and Petroleum Engineering|
|July 2014 - July 2016||Postdoctoral Fellow, NASA Goddard Space Flight Center|
|August 2011 - July 2014||Assistant Research Professor, University of Western Australia|
|July 2010 - July 2011||Research Officer, Macquarie University, Australia|
Genesis of magmatic, metasomatic and hydrothermal ore deposits in the crust and upper mantle, Metal transport by fluids in the crust and upper mantle, Fingerprinting ore-forming processes and development of innovative exploration tools, and The evolution of redox states of terrestrial planets and protoplanets
|2010||Ph.D., Macquarie University, Australia|
334 McNutt Hall
Missouri University of Science and Technology
Rolla, MO 65409
Research Works (16)
Geochronology and Geochemistry of the Intrusive Suite associated with the Khatsavch Porphyry Cu-Au (Mo) Deposit, South Mongolia Ore Geology Reviews (2019)
The Khatsavch porphyry Cu-Au (Mo) deposit is located in the Gurvansayhan island arc terrane of South Mongolia, approximately 45 km southwest of the Oyu Tolgoi Cu-Au district, one of the largest porphyry-type Cu-Au deposits in ...
Ruthenium in Chromite as Indicator for Magmatic Sulfide Liquid Equilibration in Mafic-Ultramafic Systems Ore Geology Reviews (2018)
The platinum-group element ruthenium (Ru) is an important petrogenetic tracer of Earth's accretion history, core-mantle interaction, mantle evolution and the exploration for magmatic sulfide deposits. However, its geochemical behavior in mafic-ultramafic systems is still not ...
Post-Collisional Alkaline Magmatism as Gateway for Metal and Sulfur Enrichment of the Continental Lower Crust Geochimica et Cosmochimica Acta (2018)
Mafic and ultramafic magmas that intrude into the lower crust can preserve evidence for metal and sulfur transfer from the lithospheric mantle into the lower continental crust. Here we focus on a series of ultramafic, ...
Improved Precision and Accuracy of Quantification of Rare Earth Element Abundances via Medium-Resolution LA-ICP-MS Journal of the American Society for Mass Spectrometry (2017)
Laser ablation ICP-MS enables streamlined, high-sensitivity measurements of rare earth element (REE) abundances in geological materials. However, many REE isotope mass stations are plagued by isobaric interferences, particularly from diatomic oxides and argides. In this ...
The Variability of Ruthenium in Chromite from Chassignite and Olivine-Phyric Shergottite Meteorites: New Insights into the Behavior of PGE and Sulfur in Martian Magmatic Systems Meteoritics and Planetary Science (2017)
The Martian meteorites comprise mantle-derived mafic to ultramafic rocks that formed in shallow intrusions and/or lava flows. This study reports the first in situ platinum-group element data on chromite and ulvöspinel from a series of ...
Sulfur and Metal Fertilization of the Lower Continental Crust Lithos (2016)
Mantle-derived melts and metasomatic fluids are considered to be important in the transport and distribution of trace elements in the subcontinental lithospheric mantle. However, the mechanisms that facilitate sulfur and metal transfer from the upper ...
Genesis and Tectonic Implications of Podiform Chromitites in the Metamorphosed Ultramafic Massif of Dobromirtsi (Bulgaria) Gondwana Research (2015)
Podiform chromitites occur in the meta-dunite horizon of the Dobromirtsi ultramafic massif, in the Central Rhodope metamorphic core complex (southern Bulgaria). Although these were deformed and metamorphosed together with their host rocks several chromite cores ...
The Capacity of Hydrous Fluids to Transport and Fractionate Incompatible Elements and Metals within the Earth's Mantle Geochemistry, Geophysics, Geosystems (2014)
Both silicate melts and aqueous fluids are thought to play critical roles in the chemical differentiation of the Earth's crust and mantle. Yet their relative effects are poorly constrained. We have addressed this issue by ...
Ruthenium Variation in Chromite from Komatiites and Komatiitic Basalts -- A Potential Mineralogical Indicator for Nickel Sulfide Mineralization Economic Geology (2013)
More than 390 chromite grains from komatiites and komatiitic basalts from the Yilgarn craton of Western Australia and the Finnish part of the Fennoscandian Shield were analyzed using in situ laser ablation inductively coupled plasma ...
The Oxidized Ores of the Main Sulphide Zone, Great Dyke, Zimbabwe: Turning Resources into Minable Reserves-Mineralogy Is the Key Journal of the Southern African Institute of Mining and Metallurgy (2013)
The Great Dyke of Zimbabwe constitutes the world's second largest reserve of platinum group elements (PGE) after the Bushveld Complex in neighbouring South Africa. Within the Great Dyke, economic concentrations of PGE are restricted to ...
Extremely Ni-Rich Fe-Ni Sulfide Assemblages in Komatiitic Dunite at Betheno, Western Australia: Results from Synchrotron X-ray Fluorescence Mapping Australian Journal of Earth Sciences (2011)
Fresh unserpentinised komatiitic dunite at Betheno (Western Australia) contains a distinctive sulfide assemblage of pentlandite, pyrite and millerite. The Ni tenor (i.e. Ni concentration in the original sulfide liquid) of this assemblage is in excess ...
Ruthenium in Komatiitic Chromite Geochimica et Cosmochimica Acta (2011)
The distinction between Ru in solid solution and Ru-bearing inclusions is essential for the predictive modeling of platinum-group element (PGE) geochemistry in applications such as the lithogeochemical exploration for magmatic sulfide deposits in komatiites. This ...
Cenozoic Volcanism of the Capel-Faust Basins, Lord Howe Rise, SW Pacific Ocean Deep Sea Research Part II: Topical Studies in Oceanography (2011)
New bathymetry, geophysical data and samples were acquired in 2007 during a marine reconnaissance survey using the R.V. Tangaroa in the frontier Capel and Faust basins, Lord Howe Rise (LHR) by Geoscience Australia as part ...
Erratum to Platinum-Group Element Distribution in the Oxidized Main Sulfide Zone, Great Dyke, Zimbabwe Mineralium Deposita (2010)
The online version of the original article can be found at http://dx.doi.org/10.1007/s00126-009-0258-y In the original version of this article unfortunately the first name of Frank Melcher was written incorrectly.
Platinum-Group Element Distribution in the Oxidized Main Sulfide Zone, Great Dyke, Zimbabwe Mineralium Deposita (2010)
In the Great Dyke mafic/ultramafic layered intrusion of Zimbabwe, economic concentrations of platinum-group elements (PGE) are restricted to sulfide disseminations in pyroxenites of the Main Sulfide Zone (MSZ). Oxidized ores near the surface constitute a ...
Anomalous Sulfur-Poor Platinum Group Element Mineralization in Komatiitic Cumulates, Mount Clifford, Western Australia Economic Geology (2009)
An unusual occurrence of sulfur-poor platinum group element (PGE) mineralization has been discovered at Mount Clifford in the Agnew-Wiluna belt, Western Australia, within the lower part of a 1,000-m-thick komatiitic dunite body. The host body ...