A5068039658- Hydrocarbon exploration and reservoir analysis
- Coal Properties and Utilization
- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- CO2 Sequestration and Geologic Interactions
- Methane Hydrates and Related Phenomena
- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- Atmospheric and Environmental Gas Dynamics
- Coal and Its By-products
- Geological and Geophysical Studies
- Paleontology and Stratigraphy of Fossils
- Hydraulic Fracturing and Reservoir Analysis
- Enhanced Oil Recovery Techniques
- Groundwater flow and contamination studies
- Mineral Processing and Grinding
- Mine drainage and remediation techniques
- Clay minerals and soil interactions
- Geomechanics and Mining Engineering
- Coal and Coke Industries Research
- Planetary Science and Exploration
- Rock Mechanics and Modeling
- Geological formations and processes
- Groundwater and Isotope Geochemistry
- Mining Techniques and Economics
The University of Queensland
2016-2025
Environmental Earth Sciences
1993-2023
Simon Fraser University
2023
CO2CRC
2009-2017
The University of Melbourne
2016-2017
Geological Survey of Western Australia
2001
QIMR Berghofer Medical Research Institute
1994
Queensland University of Technology
1991
Royal Children's Hospital
1991
Methanogenic and methanotrophic archaea play important roles in the global flux of methane. Culture-independent approaches are providing deeper insight into diversity evolution methane-metabolizing microorganisms, but, until now, no compelling evidence has existed for methane metabolism outside phylum Euryarchaeota. We performed metagenomic sequencing a deep aquifer, recovering two near-complete genomes belonging to archaeal Bathyarchaeota (formerly known as Miscellaneous Crenarchaeotal...
ABSTRACT Dawsonite, NaAlCO3(OH)2, is widespread as a cement, replacement, and cavity filling in Permo-Triassic sedimentary rocks of the Bowen-Gunnedah-Sydney basin system, eastern Australia. The origin dawsonite these was studied by petrographic stable isotope analysis. Dawsonite d13C (PDB) values range from -4.0 to +4.1% are remarkably consistent throughout system. These indicate either marine carbonate or magmatic source for carbon dawsonite. A considered more likely on basis that (1)...
Research Article| April 01, 2002 New evidence of magmatic-fluid–related phyllic alteration: Implications for the genesis porphyry Cu deposits Anthony C. Harris; Harris 1Department Earth Sciences, University Queensland, Queensland 4072, Australia Search other works by this author on: GSW Google Scholar Suzanne D. Golding Geology (2002) 30 (4): 335–338. https://doi.org/10.1130/0091-7613(2002)030<0335:NEOMFR>2.0.CO;2 Article history received: 26 Sep 2001 rev-recd: 16 Dec accepted: 18 first...
Research Article| July 01, 2012 U-Th dating of striated fault planes Perach Nuriel; Nuriel * 1School Earth Sciences, The University Queensland, Brisbane, QLD 4072, Australia *E-mail: pnuriel@gmail.com. Search for other works by this author on: GSW Google Scholar Gideon Rosenbaum; Rosenbaum Jian-Xin Zhao; Zhao 2Radiogenic Isotope Laboratory, Centre Microscopy and Microanalysis (CMM), Brisbane St Lucia, Yuexing Feng; Feng Suzanne D. Golding; Golding Benoît Villemant; Villemant 3Laboratoire de...
Alteration zones at the gold-rich Bajo de la Alumbrera porphyry copper deposit in northwestern Argentina are centered on several porphyritic intrusions.They zoned from a central copper-iron sulfide and gold-mineralized potassic (biotite-K-feldspar ± quartz) core outward to propylitic (chlorite-illite-epidote-calcite) assemblages.A mineralized intermediate argillic alteration assemblage (chlorite-illite pyrite) has overprinted zone across top sides of is itself into phyllic...