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Steven M. Reddy

Researcher at Curtin University

Publications -  185
Citations -  5975

Steven M. Reddy is an academic researcher from Curtin University. The author has contributed to research in topics: Zircon & Geology. The author has an hindex of 39, co-authored 168 publications receiving 4862 citations. Previous affiliations of Steven M. Reddy include University of Leeds & Australian Research Council.

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Timing of crystallization of the lunar magma ocean constrained by the oldest zircon

TL;DR: In this article, a 4417 6 Myr old zircon in lunar breccia sample 72215,195 was reported, which provides a precisely determined younger limit for the solidification of the Lunar Magma Ocean.
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Palaeoproterozoic supercontinents and global evolution: correlations from core to atmosphere

TL;DR: In this article, the authors graphically summarize the evolution from the Earth's core to its atmosphere, from the Neoarchaean to the Mesoproterozoic eras (specifically 3.0-1.2 Ga), to reveal intriguing temporal relationships across the various spheres of the Earth system.
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Quantitative characterization of plastic deformation of zircon and geological implications

TL;DR: In this article, the deformation-related microstructure of an Indian Ocean zircon hosted in a gabbro deformed at amphibolite grade has been quantified by electron backscatter diffraction.
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Crystal-plastic deformation of zircon: A defect in the assumption of chemical robustness

TL;DR: In this article, panchromatic and wavelength cathodoluminescence (CL) was combined with quantitative rare earth element (REE) ion microprobe analyses to demonstrate modification of zircon REE chemistry within the areas of crystal plasticity.
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A pressure-temperature phase diagram for zircon at extreme conditions

TL;DR: In this paper, the phase relations of ZrSiO4 polymorphs and associated dissociation products under extreme conditions using available empirical and theoretical constraints are presented. And a conceptual framework for a zircon-based approach to extreme thermobarometry that incorporates both direct observation of high-P and high-T phases, as well as inferences for the former existence of phases from orientation relationships in recrystallised products, a concept referred to here as "phase heritage".