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Norman J. Pearson

Researcher at Macquarie University

Publications -  271
Citations -  28746

Norman J. Pearson is an academic researcher from Macquarie University. The author has contributed to research in topics: Mantle (geology) & Zircon. The author has an hindex of 72, co-authored 271 publications receiving 25298 citations. Previous affiliations of Norman J. Pearson include Australian Research Council.

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The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology

TL;DR: In this paper, a laser ablation-inductively coupled plasma-mass spectrometer (LA-ICP-MS) was used for in situ U-Pb zircon geochronology.
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The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites

TL;DR: In this article, the isotopic composition of Hf has been measured in 124 mantle-derived zircon megacrysts from African, Siberian and Australian kimberlites, using a laser-ablation microprobe (LAM) and a multi-collector ICPMS.
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Zircon chemistry and magma mixing, SE China: In-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes

TL;DR: In this article, in-situ LAM-MC-ICPMS microanalysis shows large variations in 176Hf/177Hf (up to 15 eHf units) between zircons of different growth stages within a single rock, and between zones within single zircon grains, suggesting that each of the observed magmas in both complexes developed through hybridisation of ≥2 magmas with different sources.
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Archean crustal evolution in the northern Yilgarn Craton: U–Pb and Hf-isotope evidence from detrital zircons

TL;DR: Whitaker et al. as mentioned in this paper integrated U-Pb dating, Hf-isotope analysis and trace-element analysis to detrital zircon populations offers a rapid means of assessing the geochronology and crustal evolution history of different terranes within a composite craton.
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The growth of the continental crust: Constraints from zircon Hf-isotope data

TL;DR: In this paper, the authors introduce a new approach to quantitatively estimate the proportion of juvenile material added to the crust at any given time during its evolution, which is then used to model the crustal growth rate over the 4.56-Ga of Earth's history.