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Simon Chenery

Researcher at British Geological Survey

Publications -  131
Citations -  4031

Simon Chenery is an academic researcher from British Geological Survey. The author has contributed to research in topics: Inductively coupled plasma mass spectrometry & Laser ablation. The author has an hindex of 34, co-authored 123 publications receiving 3586 citations. Previous affiliations of Simon Chenery include University of Manchester & Imperial College London.

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Sources and uptake of trace metals in otoliths of juvenile barramundi (Lates calcarifer)

TL;DR: Under experimental conditions, otolith concentrations of several trace metals are related to water concentrations, however, these patterns do not simply extrapolate to the natural environment where the mechanisms involved appear to be more complex.
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Contrasted monazite hydrothermal alteration mechanisms and their geochemical implications

TL;DR: In this article, an integrated study involving backscattered scanning electron microscopy, electron microprobe analyses, and laser ablation-inductively coupled plasma mass spectrometry (LA-ICP-MS) reveals that the chloritization event was characterized by the coupled substitution 2REE3+ ⇌ Th4+ + + Ca2+ in the altered parts of the monazite, thus leaving the P-O framework of the crystal untouched.
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Electron microprobe and LA-ICP-MS study of monazite hydrothermal alteration: Implications for U-Th-Pb geochronology and nuclear ceramics

TL;DR: In this paper, the authors quantify the response of magmatic monazite to three main types of hydrothermal alteration, namely sericitization, chloritization, and greisenization, using backscattered scanning electron microscopy (BSE-SEM), electron microprobe, laser Raman spectroscopy and laser ablation-inductively coupled plasma-mass spectrometry.
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The generation of prograde P T t points and paths; a textural, compositional, and chronological study of metamorphic monazite

TL;DR: In this paper, an approach that allows multiple prograde pressure-temperature-time (P-T-t) points to be generated on single samples providing a means to construct detailed P-T -t loops, enabling the duration of metamorphic events, the timing of burial and the rate of heating experienced by individual samples to be determined.