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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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Disequilibrium melting during crustal anatexis and implications for modeling open magmatic systems

TL;DR: In this paper, a suite of volcanic rocks and entrained crustal xenoliths from the Central Andes using bulk geochemical compositions for mantle-derived and crustal end-members was investigated and modeled for a suite with respect to the continental crust.
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Moving peoples, changing diets: Isotopic differences highlight migration and subsistence changes in the Upper Mun River Valley, Thailand

TL;DR: In this paper, the authors used isotope analysis to examine the human skeletal remains from Ban Non Wat, northeast Thailand, to give insight into patterns of migration and subsistence strategy during prehistory.
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Quantitative analysis of trace element concentrations in some gem-quality diamonds.

TL;DR: A new ICPMS-based (ICPMS: inductively coupled plasma mass spectrometry) method for the analysis of trace element concentrations within fluid-poor, gem-quality diamonds is presented, providing some supporting evidence of a link between the parental fluids for both fluid-inclusion-rich and gem diamonds.
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Isotopic investigation of diet and residential mobility in the Neolithic of the Lower Rhine Basin.

TL;DR: In this article, carbon and nitrogen isotope analyses of European Mesolithic and Neolithic populations showed a shift in diet from the Mesolithic to the Neolithic, but also great variety in Neolithic diets, several of which incorporate fish.
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Extensive crustal extraction in Earth’s early history inferred from molybdenum isotopes

TL;DR: In this paper, the authors present molybdenum isotope data for Archaean komatiites and Phanerozoic komatisites and picrites and demonstrate that their mantle sources all possess subchondritic signatures complementary to the superchondrich continental crust.