Artur P. Deditius

ORCID: 0000-0001-8601-2544
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • Metal Extraction and Bioleaching
  • Radioactive element chemistry and processing
  • Minerals Flotation and Separation Techniques
  • Geochemistry and Elemental Analysis
  • Nuclear materials and radiation effects
  • Geomagnetism and Paleomagnetism Studies
  • Extraction and Separation Processes
  • Mine drainage and remediation techniques
  • Mineral Processing and Grinding
  • earthquake and tectonic studies
  • Clay minerals and soil interactions
  • Arsenic contamination and mitigation
  • Mineralogy and Gemology Studies
  • Nuclear Materials and Properties
  • Iron oxide chemistry and applications
  • Paleontology and Stratigraphy of Fossils
  • Geology and Paleoclimatology Research
  • Geophysical and Geoelectrical Methods
  • High-pressure geophysics and materials
  • Hydrocarbon exploration and reservoir analysis
  • Adsorption and biosorption for pollutant removal
  • Calcium Carbonate Crystallization and Inhibition
  • Heavy metals in environment

Murdoch University
2015-2024

The University of Western Australia
2022-2024

Graz University of Technology
2010-2015

Commonwealth Scientific and Industrial Research Organisation
2009

University of Michigan
2006-2009

Research Article| July 01, 2015 Giant Kiruna-type deposits form by efficient flotation of magmatic magnetite suspensions Jaayke L. Knipping; Knipping * 1Department Earth and Environmental Sciences, University Michigan, 1100 North Avenue, Ann Arbor, Michigan 48109-1005, USA *E-mail: jaaykek@umich.edu Search for other works this author on: GSW Google Scholar Laura D. Bilenker; Bilenker Adam C. Simon; Simon Martin Reich; Reich 2Department Geology Andean Geothermal Center Excellence (CEGA),...

10.1130/g36650.1 article EN Geology 2015-05-20

Although studies have proposed that iron oxide-apatite (IOA) deposits may represent the deeper roots of some Andean oxide copper-gold (IOCG) systems, their genetic links remain obscure and controversial. A key question when considering an integrated model is whether a magmatic-hydrothermal fluid precipitates massive magnetite will continue transporting significant amounts dissolved Fe, Cu, Au after IOA precipitation. Here we provide new geochemical data for accessory pyrite from Los...

10.2113/econgeo.111.3.743 article EN Economic Geology 2016-04-08

Research Article| August 01, 2009 Decoupled geochemical behavior of As and Cu in hydrothermal systems Artur P. Deditius; Deditius 1Department Geological Sciences, University Michigan, Ann Arbor, Michigan 48109-1005, USA2Commonwealth Scientific Industrial Organisation (CSIRO), Exploration Mining, 26 Dick Perry Avenue, Perth, WA 6151, Australia Search for other works by this author on: GSW Google Scholar Satoshi Utsunomiya; Utsunomiya 3Kyushu University, Department Chemistry, Ropponmatsu,...

10.1130/g25781a.1 article EN Geology 2009-07-30

Abstract The genetic link between magmas and ore deposit formation is well documented by studies of fossil hydrothermal systems associated with magmatic intrusions at depth. However, the role explosive volcanic processes as active agents mineralization remains unexplored owing to fact that metals volatiles are released into atmosphere during eruption arc volcanoes. Here, we draw on observations uniquely preserved El Laco iron in Central Andes shed new light metallogenic volcanism operates a...

10.1038/s41598-018-33206-3 article EN cc-by Scientific Reports 2018-10-01

Arsenic-rich (arsenian) pyrite can contain up to tens of thousands parts per million (ppm) toxic heavy metals such as Hg, Tl, and Cd, although few data are available on their solid solubility behavior. When a compilation Cd analyses from different environments plotted along with As in M(Hg, Cd)-As log-log space, the resulting wedge-shaped distribution points suggests that aforementioned is strongly dependent concentration pyrite. The limits Hg arsenian pyrite—i.e., upper limit zone...

10.2138/am-2016-5603 article EN American Mineralogist 2016-06-01

A new mode of arsenic incorporation into arsenian pyrite has been discovered. Electron microprobe analyses and elemental maps from Pueblo Viejo, Dominican Republic, show that its chemical composition varies (Fe0.998As0.003)1.001S2 to (Fe0.963As0.050Cu0.003Ag0.001)1.017S2 is inversely correlated with Fe. High-resolution transmission electron microscopy (HRTEM) images some in this present as nanoscale inclusions amorphous As- Fe-S a matrix pyrite. The display negative facets cubic or...

10.2138/am.2009.3116 article EN American Mineralogist 2009-02-01
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