Chris Clark
geology.curtin.edu.au
0000-0001-9982-7849
Curtin University
99 papers found
Refreshing results…
Probing the history of ultra‐high temperature metamorphism through rare earth element diffusion in zircon
Petrographically-controlled elemental mobility in monazite and rutile in ultrahigh temperature granulites
Persistence of melt-bearing Archean lower crust for >200 m.y.— An example from the Lewisian Complex, northwest Scotland
Titanite dates crystallization: Slow Pb diffusion during super‐solidus re‐equilibration
The Neoarchean Uyea Gneiss Complex, Shetland: an onshore fragment of the Rae Craton on the European Plate
Testing the fidelity of thermometers at ultrahigh temperatures
Closed system behaviour of argon in osumilite records protracted high‐Tmetamorphism within the Rogaland–Vest Agder Sector, Norway
Neoproterozoic hydrothermal activity in the West Australian Craton related to Rodinia assembly or breakup?
A window into an ancient backarc? The magmatic and metamorphic history of the Fraser Zone, Western Australia
Analysis of Natural Rutile (TiO2) by Laser-assisted Atom Probe Tomography
Unravelling complex geologic histories using U–Pb and trace element systematics of titanite
First Precambrian palaeomagnetic data from the Mawson Craton (East Antarctica) and tectonic implications
Footprint of a large intracontinental rifting event: Coupled detrital zircon geochronology and geochemistry from the Mesoproterozoic Collier Basin, Western Australia
Neoproterozoic evolution and Cambrian reworking of ultrahigh temperature granulites in the Eastern Ghats Province, India
A tripartite approach to unearthing the duration of high temperature conditions versus peak metamorphism: An example from the Bunger Hills, East Antarctica
Isotopic constraints on fluid evolution and ore precipitation in a sediment-hosted Pb-Ag-Ba-Zn-Cu-Au deposit in the Capricorn Orogen, Western Australia
Prolonged (>100 Ma) ultrahigh temperature metamorphism in the Napier Complex, East Antarctica: A petrochronological investigation of Earth's hottest crust
In situ U-Pb geochronology and geochemistry of a 1.13 Ga mafic dyke suite at Bunger Hills, East Antarctica: The end of the Albany-Fraser Orogeny
Th/U ratios in metamorphic zircon
Extensional episodes in the Paleoproterozoic Capricorn Orogen, Western Australia, revealed by petrogenesis and geochronology of mafic–ultramafic rocks
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