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Low {delta}{sup 18}O magma, Isle of Skye, Scotland: Evidence from zircons

Journal Article · · Geochimica et Cosmochimica Acta
;  [1]
  1. Univ. of Wisconsin, Madison, WI (United States)

Zircons in Tertiary granitic rocks from the Isle of Skye, Scotland were resistant to measurable oxygen isotope exchange during intense hydrothermal activity in the subvolcanic environment. Five granite bodies from the Western Red Hills complex were investigated; four have {sup 18}O (Zrc) = 4.1 {+-} 0.2{per_thousand} (VSMOW) while the fifth, which intruded before major cauldron subsidence, is 2{per_thousand} lower. Zircons from Lewisian gneiss are visually and isotopically distinct indicating that zircons in the granite are not xenocrysts from the Lewisian basement. Analysis of different magnetic and size fractions of zircon shows no significant correlation to {delta}{sup 18}O supporting the conclusion that these values represent the true magmatic compositions and that the Western Red Hills granites intruded as low {delta}{sup 18}O magmas with a whole rock {delta}{sup 18}O {le} 6.0%. Quartz separates from four granites are close to the calculated magmatic values in {delta}{sup 18}O, but in the fifth, values are 5% lower indicating variable exchange of quartz with low {delta}{sup 18}O heated meteoric waters. These results might be explained by magmatic interaction with hydrothermally altered crust early in the evolution of the granites, before crystallization of zircon, followed by interaction with later hydrothermal fluids. Alternatively, independent evidence for low {delta}{sup 18}O mafic magmatism in NW Scotland suggests the presence of large quantities of low {delta}{sup 18}O subducted ocean crust in the subcontinental lithosphere that could contaminate or be the source of low {delta}{sup 18}O mantle-derived melts. 31 refs., 4 figs., 1 tab.

DOE Contract Number:
FG02-93ER14389
OSTI ID:
617825
Journal Information:
Geochimica et Cosmochimica Acta, Journal Name: Geochimica et Cosmochimica Acta Journal Issue: 23 Vol. 61; ISSN 0016-7037; ISSN GCACAK
Country of Publication:
United States
Language:
English

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