F
Finlay M. Stuart
Researcher at Scottish Enterprise
Publications - 214
Citations - 7150
Finlay M. Stuart is an academic researcher from Scottish Enterprise. The author has contributed to research in topics: Mantle (geology) & Basalt. The author has an hindex of 45, co-authored 193 publications receiving 6176 citations. Previous affiliations of Finlay M. Stuart include Chinese Academy of Sciences & University of Manchester.
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High 3He/4He ratios in picritic basalts from Baffin Island and the role of a mixed reservoir in mantle plumes.
TL;DR: It is shown that olivine phenocrysts in picritic basalts presumably derived from the proto-Iceland plume at Baffin Island, Canada, have the highest magmatic 3He/4He ratios yet recorded, indicating that a 3He-recharged depleted mantle (HRDM) reservoir may be the principal source of high 3He /4He in mantle plumes.
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Resolving mantle and crustal contributions to ancient hydrothermal fluids: HeAr isotopes in fluid inclusions from Dae Hwa WMo mineralisation, South Korea
TL;DR: In this article, a large scheelite crystal from the 88 Ma Dae Hwa WMo deposit, South Korea, was used to trace the source and history of the ore fluids.
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Formation of hybrid arc andesites beneath thick continental crust
Susanne M. Straub,Susanne M. Straub,Arturo Gómez-Tuena,Finlay M. Stuart,Georg F. Zellmer,Ramon Espinasa-Perena,Yue Cai,Yue Cai,Yoshiyuki Iizuka +8 more
TL;DR: This article used 3He/4He ratios of high-Ni olivines to demonstrate the mantle origin of basaltic to andesitic arc magmas in the central Mexican Volcanic Belt (MVB).
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Noble gases confirm plume-related mantle degassing beneath Southern Africa.
Stuart Gilfillan,Domokos Györe,Stephanie Flude,Stephanie Flude,Gareth Johnson,Clare E. Bond,Nigel Hicks,Robert Lister,David G. Jones,Yannick Kremer,R. S. Haszeldine,Finlay M. Stuart +11 more
TL;DR: It is shown that natural CO2 seeps along the Ntlakwe-Bongwan fault within KwaZulu-Natal, South Africa, have C-He isotope systematics that support an origin from degassing mantle melts, confirming plume-related mantle melting.
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A Devonian auriferous hot spring system, Rhynie, Scotland
Clive Maitland Rice,W. A. Ashcroft,David J. Batten,Adrian J. Boyce,J. B. D. Caulfield,Anthony E. Fallick,Malcolm J. Hole,E. Jones,Michael J. Pearson,Graeme Rogers,J. M. Saxton,Finlay M. Stuart,Nigel H. Trewin,Grenville Turner +13 more
TL;DR: The Early Devonian Rhynie hot spring system is the oldest known and is of the low sulphidation type as mentioned in this paper, it extends for at least 1.5 km along a major fault zone defining the western margin of an outlier of fluvial and lacustrine sediments, plant-bearing sinters and andesitic lavas.