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Reid R. Keays

Researcher at Monash University

Publications -  157
Citations -  10576

Reid R. Keays is an academic researcher from Monash University. The author has contributed to research in topics: Basalt & Ultramafic rock. The author has an hindex of 60, co-authored 156 publications receiving 9965 citations. Previous affiliations of Reid R. Keays include University of Chicago & University of Melbourne.

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Effects of Chemical Weathering and Sorting on the Petrogenesis of Siliciclastic Sediments, with Implications for Provenance Studies

TL;DR: The bulk chemical compositions, mineralogy, and mineral proportions of sands and muds of the Mallacoota Basin in southeastern Australia reflect the composition of weathering profiles mantling source rocks, rather than bedrock as discussed by the authors.
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A temporal link between the Emeishan large Igneous Province (SW China) and the end-Guadalupian mass extinction

TL;DR: Using the Sensitive High-Resolution Ion Microprobe to analyze zircons, this paper established the age of the Xinjie intrusion, believed to be a feeder to the main phase of Emeishan flood basalt (EFB) volcanism, to be 259±3 Ma.
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The role of komatiitic and picritic magmatism and S-saturation in the formation of ore deposits

TL;DR: The link between komatiitic and picritic magmatism and mineralization is not as clear cut in the case of the Noril'sk Cu-Ni-PGE deposits, but nevertheless there is an association between the two types of magmas and ore deposit development.
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Sulfide melt-silicate melt distribution coefficients for noble metals and other chalcophile elements as deduced from MORB: Implications for partial melting

TL;DR: In this article, an analysis of chalcophile elements in coexisting sulfide and glass of basalts from the FAMOUS area of the mid-Atlantic ridge has been obtained by combined instrumental and radiochemical neutron activation analysis and directly coupled plasma spectrometry of hand-picked separates.
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Geochemistry, Petrogenesis and Metallogenesis of the Panzhihua Gabbroic Layered Intrusion and Associated Fe-Ti-V Oxide Deposits, Sichuan Province, SW China

TL;DR: The Panzhihua gabbroic layered intrusion is associated with the 260Ma Emeishan Large Igneous Province in SW China as discussed by the authors, which hosts a giant Fe-Ti-V oxide deposit with 1333 million ton ore reserves.