Terrence P. Mernagh

ORCID: 0000-0002-8555-0110
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Hydrocarbon exploration and reservoir analysis
  • Electrochemical Analysis and Applications
  • Mineralogy and Gemology Studies
  • Gold and Silver Nanoparticles Synthesis and Applications
  • Glass properties and applications
  • Geochemistry and Elemental Analysis
  • Geology and Paleoclimatology Research
  • Geological and Geophysical Studies
  • Clay minerals and soil interactions
  • Ion-surface interactions and analysis
  • Diamond and Carbon-based Materials Research
  • CO2 Sequestration and Geologic Interactions
  • Electron and X-Ray Spectroscopy Techniques
  • Radioactive element chemistry and processing
  • Crystal Structures and Properties
  • Mineral Processing and Grinding
  • Electronic and Structural Properties of Oxides
  • Methane Hydrates and Related Phenomena
  • X-ray Spectroscopy and Fluorescence Analysis
  • Mining Techniques and Economics
  • Laser-induced spectroscopy and plasma

Australian National University
2015-2025

Institute of Geochemistry
2019-2022

Chinese Academy of Sciences
2019-2022

Geoscience Australia
2006-2019

Geological Survey of Western Australia
1993-2002

Mineral Resources
1987-1993

University of Newcastle Australia
1981-1985

Nondestructive proton-induced X-ray emission (PIXE) analysis is used to measure the concentrations of base metals and other heavy elements in single hypersaline brine inclusions low-salinity vapor inclusions, which are intimately associated within a granite-hosted quartz-cassiterite vein Mole Granite (New South Wales, eastern Australia). Microther-mometric measurements Raman microspectrometry on same complement data.The have an estimated composition (in wt %): NaCl, 20; KCl, 7; CaCl 2 , 0.9;...

10.2113/gsecongeo.87.6.1566 article EN Economic Geology 1992-10-01

Research Article| February 01, 2006 Gold and metal enrichment in natural granitic melts during fractional crystallization Roger Mustard; Mustard 1Predictive Mineral Discovery Cooperative Centre, Economic Geology Unit, School of Earth Sciences, James Cook University, Townsville, QLD 4811, Australia Search for other works by this author on: GSW Google Scholar Thomas Ulrich; Ulrich 2Earth Marine Science Department, Australian National Canberra, ACT 0200, Vadim S. Kamenetsky; Kamenetsky 3School...

10.1130/g22141.1 article EN Geology 2006-01-01

Abstract The S anshandao gold deposit, located at northwestern edge of the J iaodong P eninsula, eastern N orth C hina raton, is one largest deposits in province. In disseminated‐ and stockwork‐style ores are hosted M esozoic granitoids. Mineralization alteration largely controlled by regional anshandao– angshang fault. Sericite separated from rocks mineralized zone yields an Rb–Sr isochron age 117.6 ± 3.0 Ma. ore‐forming fluids deposit contain CO 2 ‐H O‐NaCl±CH 4 with low to intermediate...

10.1111/gfl.12065 article EN Geofluids 2013-09-16

Kiruna-type iron oxide-apatite (IOA) deposits, an important source of iron, show close associations with andesitic subvolcanic intrusions. However, the processes ore formation and mechanism controlling concentration remain uncertain. Here, we report widespread presence high-temperature (>800°C) water-poor multisolid hydrosaline liquid inclusions in pre- syn-ore minerals from IOA deposits eastern China. These consistently homogenize to a phase by vapor disappearance mostly contain 3 10 wt %...

10.1126/sciadv.adk2174 article EN cc-by-nc Science Advances 2024-04-24

Abstract Raman spectroscopy was used to distinguish the individual members of two feldspar subgroups. All feldspars were found exhibit a characteristic, intense line between 500 and 515 cm −1 which is attributed mixed SiOSi (or SiOAl) bending/stretching mode. However, discrimination related within each subgroup relies on change in frequencies band widths occur external lattice modes SiO stretching region. Spectra recorded from single crystals powders demonstrate that laser microprobe...

10.1002/jrs.1250220806 article EN Journal of Raman Spectroscopy 1991-08-01

The world’s most ancient biogenic structures are found in the North Pole Dome of Western Australia, where 3.47-Gyr-old algal mats and stromatolites closely associated with bedding-conformable discordant laminar quartz, chalcedony, barite. Barite-rich quartz hydrothermal veins similar mineralogy occur throughout stratigraphy below conformable structures. With exception large volume barite, these exhibit textures alteration (quartz-chalcedony-chlorite-illite ± calcite-adularia-pyrite) typical...

10.2113/gsecongeo.104.6.793 article EN Economic Geology 2009-09-01

Research Article| November 01, 2018 Gas–Solid Reactions: Theory, Experiments and Case Studies Relevant to Earth Planetary Processes Penelope L. King; King School of Sciences, The Australian National University, Canberra ACT 2601 Australia Search for other works by this author on: GSW Google Scholar Vincent M. Wheeler; Wheeler Engineering, Christian J. Renggli; Renggli Andrew B. Palm; Palm Siobhan A. Wilson; Wilson Department Atmospheric University Alberta, Edmonton, AB T6G 2E3 Canada Anna...

10.2138/rmg.2018.84.1 article EN Reviews in Mineralogy and Geochemistry 2018-11-01

We reinterpret the regional geologic setting of giant Muruntau gold deposit and report new 40 Ar/ 39 Ar isotope age determinations a laser Raman microprobe analysis fluid inclusions. New hydrothermal sericite selvages to gold-stage quartz veins are in excellent agreement with older Rb-Sr dates on auriferous veins. They suggest Triassic formation at 245 220 Ma, some 30 m.y. later than subjacent felsic intrusions as defined by data. These call into question role magmatic fluid, metal, heat...

10.2113/gsecongeo.96.3.633 article EN Economic Geology 2001-05-01

Research Article| August 01, 1999 Volatile exsolution at the Dinkidi Cu-Au porphyry deposit, Philippines: A melt-inclusion record of initial ore-forming process Vadim S. Kamenetsky; Kamenetsky 1School Earth Sciences and Centre for Ore Deposit Research, University Tasmania, GPO Box 252-79, Hobart, Tasmania 7001, Australia Search other works by this author on: GSW Google Scholar Rohan C. Wolfe; Wolfe Stephen M. Eggins; Eggins 2Department Geology, Australian National University, Canberra ACT...

10.1130/0091-7613(1999)027<0691:veatdc>2.3.co;2 article EN Geology 1999-01-01

10.1016/0168-583x(91)95528-l article EN Nuclear Instruments and Methods in Physics Research Section B Beam Interactions with Materials and Atoms 1991-03-01

Research Article| November 01, 2001 Melt inclusion record of immiscibility between silicate, hydrosaline, and carbonate melts: Applications to skarn genesis at Mount Vesuvius Paolo Fulignati; Fulignati 1Dipartimento di Scienze della Terra, Università degli Studi Pisa, via Santa Maria 53, 56126 Italy Search for other works by this author on: GSW Google Scholar Vadim S. Kamenetsky; Kamenetsky 2School Earth Sciences Centre Ore Deposit Research, University Tasmania, GPO Box 252-79, Hobart,...

10.1130/0091-7613(2001)029<1043:miroib>2.0.co;2 article EN Geology 2001-01-01

Research Article| May 01, 2002 Extreme chemical heterogeneity of granite-derived hydrothermal fluids: An example from inclusions in a single crystal miarolitic quartz Vadim S. Kamenetsky; Kamenetsky 1School Earth Sciences and Centre for Ore Deposit Research, University Tasmania, GPO Box 252-79, Hobart, TAS 7001, Australia Search other works by this author on: GSW Google Scholar Esme van Achterbergh; Achterbergh 2Commonwealth Scientific Industrial Organisation—Exploration Mining, P.O. 136,...

10.1130/0091-7613(2002)030<0459:echogd>2.0.co;2 article EN Geology 2002-01-01

Studies of liquid-vapor-multisolid (L-V-nS) and liquid-vapor ± halite fluid inclusions suggest that at least three fundamentally different brines were involved in the genesis Proterozoic ironstone-hosted Starra Au-Cu deposit. Element concentrations determined from proton-induced X-ray emission (PIXE) analysis groups L-V-nS early barren magnetite ironstone stage (400°–550°C) younger mineralization (220°–360°C) covary over concentration ranges greater than deduced analytical errors. The two...

10.2113/gsecongeo.96.4.875 article EN Economic Geology 2001-07-01

This study reports results of mass transfer calculations using chemical modeling software (HCh) to determine parameters that may have had a significant effect on gold deposition in turbidite-hosted Phanerozoic metamorphic terranes. The system modeled was Al-As-Au-C-Ca-Cl-Cu-Fe-H-K-Mg-N-Na-O-S-Sb-Si simulate fluid-rock interaction, gas partitioning, and mineral precipitation veins. Each run takes into consideration both (1) the composition vein fluid minerals predicted precipitate (2) fluids...

10.2113/gsecongeo.103.8.1613 article EN Economic Geology 2008-12-01
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