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Dive into the research topics where Angela Halfpenny is active.

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Featured researches published by Angela Halfpenny.


American Mineralogist | 2015

Microelectronic junctions in arsenian pyrite due to impurity and mixed sulfide heterogeneity

Jamie S. Laird; Colin M. MacRae; Angela Halfpenny; Rr Large; C.G. Ryan

Abstract Impurities and crystal defects within the semiconducting bulk of a metal sulfide introduce energy levels within the forbidden bandgap. These levels in turn control semiconducting type and local electrical properties within single and multi-phased sulfide assemblages. Heterogeneity in sulfide semiconductivity linked to these impurities can lead to p-n micro-junction formation and potential distributions near the surface that may alter redox reactivity. Secondary gold ore genesis via a micro-galvanic effect related to heterogeneity has in the past been hypothetically linked to such micro-junctions. Understanding these regions and their interaction with weathering fluids in the regolith for example requires large-scale imaging of potential distributions associated with near-surface micro-junctions and correlation with the responsible elemental distributions. Here we investigate the existence of micro-electronic junctions in a mixed sulfide assemblage using scanning laser beam induced current (LBIC) and correlate them with pyrite-chalcopyrite interfaces mapped using combined energy-dispersive spectroscopy (EDS) and wavelength-dispersive spectroscopy (WDS) on an electron hyper-probe. Junctions in a natural assemblage are positively identified for the first time.


Materials Science Forum | 2013

Crystallography of Natural and Synthetic Gold Alloy Microstructures

Angela Halfpenny; Robert M. Hough; Michael Nugus

To improve our understanding of the mechanisms of gold deposition, a comparison was made of the microstructures of a natural gold sample with a synthetic gold foil of similar alloy composition (approximately Au 90%, Ag 10%). The aim was to identify any similarities between the samples that could help increase our knowledge of how the natural gold microstructures formed and were modified post-mineralisation. The samples were analysed using electron backscatter diffraction to map their microstructure, with the synthetic gold foil then heated to and mapped at 400°C, 500°C, 600°C and 700°C. Both the natural and synthetic sample exhibited a dominance of ∑3 twin boundaries, but these were much less abundant in the synthetic sample prior to heating. The natural sample is dominated by coarse grains exhibiting lattice distortion and low angle grain boundaries, which more closely resemble the synthetic gold foil microstructure after recrystallisation has taken place, than the initial microstructure, implying that the grains have had time to grow. Performing experiments such as these allows direct comparison of gold microstructures where the formation conditions are known and the controlling mechanisms can be determined. This will improve our understanding of the important mechanisms behind gold deposition.


Journal of Metamorphic Geology | 2011

Garnet re-equilibration by coupled dissolution–reprecipitation: evidence from textural, major element and oxygen isotope zoning of ‘cloudy’ garnet

Laure Martin; Michel Ballèvre; Philippe Boulvais; Angela Halfpenny; Olivier Vanderhaeghe; Sylvain Duchene; Etienne Deloule


Mineralium Deposita | 2015

Quantified, multi-scale X-ray fluorescence element mapping using the Maia detector array: application to mineral deposit studies

Louise Fisher; Denis Fougerouse; James S. Cleverley; C.G. Ryan; Steven Micklethwaite; Angela Halfpenny; Robert M. Hough; M.A.M. Gee; David Paterson; Daryl L. Howard; Kathryn Spiers


Geochimica et Cosmochimica Acta | 2016

Gold remobilisation and formation of high grade ore shoots driven by dissolution-reprecipitation replacement and Ni substitution into auriferous arsenopyrite

Denis Fougerouse; Steven Micklethwaite; Andrew George Tomkins; Yuan Mei; Matt R. Kilburn; Paul Guagliardo; Louise Fisher; Angela Halfpenny; M.A.M. Gee; David Paterson; Daryl L. Howard


Terra Nova | 2016

The golden ark: Arsenopyrite crystal plasticity and the retention of gold through high strain and metamorphism

Denis Fougerouse; Steven Micklethwaite; Angela Halfpenny; Steven M. Reddy; John Cliff; Laure Martin; Matt R. Kilburn; Paul Guagliardo; Stanislav Ulrich


Geochimica et Cosmochimica Acta | 2013

LA-ICP-MS mapping of olivine from the Brahin and Brenham meteorites: Complex elemental distributions in the pallasite olivine precursor

Seann J. McKibbin; Hugh St. C. O’Neill; Guilherme Mallmann; Angela Halfpenny


Ore Geology Reviews | 2017

Actively forming Kuroko-type volcanic-hosted massive sulfide (VHMS) mineralization at Iheya North, Okinawa Trough, Japan

Christopher J. Yeats; Steven P. Hollis; Angela Halfpenny; Juan Carlos Corona; Crystal LaFlamme; Gordon Southam; Marco L. Fiorentini; Richard J. Herrington; John Spratt


Meteoritics & Planetary Science | 2016

Characterization of Mason Gully (H5): The second recovered fall from the Desert Fireball Network

Kathryn A. Dyl; G. K. Benedix; P. A. Bland; Jon M. Friedrich; Pavel Spurný; Martin C. Towner; Mary Claire O'Keefe; K. T. Howard; R. C. Greenwood; Robert J. Macke; Daniel T. Britt; Angela Halfpenny; James O. Thostenson; Rebecca A. Rudolph; Mark L. Rivers; A. W. R. Bevan


Lithos | 2015

The structure of and origin of nodular chromite from the Troodos ophiolite, Cyprus, revealed using high-resolution X-ray computed tomography and Electron Backscatter Diffraction.

Hazel Margaret Prichard; Sarah-Jane Barnes; Bélinda Godel; Steven M. Reddy; Z. Vukmanovic; Angela Halfpenny; C. Neary; Peter Charles Fisher

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Steven Micklethwaite

University of Western Australia

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Matt R. Kilburn

University of Western Australia

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Robert M. Hough

Commonwealth Scientific and Industrial Research Organisation

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C.G. Ryan

Commonwealth Scientific and Industrial Research Organisation

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Laure Martin

University of Western Australia

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Louise Fisher

Commonwealth Scientific and Industrial Research Organisation

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M.A.M. Gee

University of Western Australia

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