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Geoff Nowell

Researcher at Durham University

Publications -  124
Citations -  7418

Geoff Nowell is an academic researcher from Durham University. The author has contributed to research in topics: Mantle (geology) & Kimberlite. The author has an hindex of 42, co-authored 118 publications receiving 6600 citations. Previous affiliations of Geoff Nowell include University of Nottingham & Instituto Superior Técnico.

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The behavior of iron and zinc stable isotopes accompanying the subduction of mafic oceanic crust: A case study from Western Alpine ophiolites

TL;DR: In this paper, the chemistry and oxidation state of fluids released during prograde metamorphism of subducted oceanic crust was investigated using metagabbros and metabasalts from the Chenaillet massif, Queyras complex and Zermatt-Saas ophiolite.
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Kimberlites reveal 2.5-billion-year evolution of a deep, isolated mantle reservoir

TL;DR: Gl Globally distributed kimberlites have their origins in a single, homogeneous early Earth reservoir that was subsequently perturbed, probably by subduction along the margins of Pangaea, around 200 million years ago, revealing a long-lived and globally extensive mantle reservoir that underwent subsequent disruption.
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Sr isotope analysis of bird feathers by TIMS: a tool to trace bird migration paths and breeding sites

TL;DR: In this paper, the Sedge Warbler (Acrocephalus schoenobaenus) feathers were used from four different locations within Europe and the shaft and the vane parts of the feather were analysed separately.
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Origin of CFB Magmatism: Multi-tiered Intracrustal Picrite^Rhyolite Magmatic Plumbing at Spitzkoppe, Western Namibia, during Early Cretaceous Etendeka Magmatism

TL;DR: Early Cretaceous tholeiitic picrite-to-rhyolite dykes around Spitzkoppe, western Namibia, are part of the extensive Henties Bay-Outjo swarm, penecontemporaneous with 132 Ma Etendeka lavas 100 km to the NW as mentioned in this paper.
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From source to crust: Tracing magmatic evolution in a kimberlite and a melilitite using microsample geochemistry

TL;DR: In this paper, an integrated micro-sampling trace element and isotopic study of primary minerals within the Jos kimberlite, Canada, in order to observe how different phases record progressive crustal interaction in the evolving kimbersite.