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Trace element and isotope constraints on crustal anatexis by upwelling mantle melts in the North Atlantic Igneous Province: an example from the Isle of Rum, NW Scotland

Published online by Cambridge University Press:  27 February 2009

ROMAIN MEYER ,
GRAEME R. NICOLL ,
JAN HERTOGEN ,
VALENTIN R. TROLL ,
ROBERT M. ELLAM  and
C. HENRY EMELEUS
ROMAIN MEYER
Affiliation:
Geo-Instituut, Katholieke Universiteit Leuven, Celestijnenlaan 200E, B-3001 Leuven-Heverlee, Belgium
GRAEME R. NICOLL
Affiliation:
Department of Geology, University of Dublin, Trinity College, Dublin 2, Ireland
JAN HERTOGEN*
Affiliation:
Geo-Instituut, Katholieke Universiteit Leuven, Celestijnenlaan 200E, B-3001 Leuven-Heverlee, Belgium
VALENTIN R. TROLL
Affiliation:
Department of Geology, University of Dublin, Trinity College, Dublin 2, Ireland
ROBERT M. ELLAM
Affiliation:
Scottish Universities Environmental Research Centre, Rankine Ave., East Kilbride G75 0QF, UK
C. HENRY EMELEUS
Affiliation:
Department of Earth Sciences, University of Durham, Durham DH1 3LE, UK
*
‡Author for correspondence: [email protected]
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Abstract

Sr and Nd isotope ratios, together with lithophile trace elements, have been measured in a representative set of igneous rocks and Lewisian gneisses from the Isle of Rum in order to unravel the petrogenesis of the felsic rocks that erupted in the early stages of Palaeogene magmatism in the North Atlantic Igneous Province (NAIP). The Rum rhyodacites appear to be the products of large amounts of melting of Lewisian amphibolite gneiss. The Sr and Nd isotopic composition of the magmas can be explained without invoking an additional granulitic crustal component. Concentrations of the trace element Cs in the rhyodacites strongly suggests that the gneiss parent rock had experienced Cs and Rb loss prior to Palaeogene times, possibly during a Caledonian event. This depletion caused heterogeneity with respect to 87Sr/86Sr in the crustal source of silicic melts. Other igneous rock types on Rum (dacites, early gabbros) are mixtures of crustal melts and and primary mantle melts. Forward Rare Earth Element modelling shows that late stage picritic melts on Rum are close analogues for the parent melts of the Rum Layered Suite, and for the mantle melts that caused crustal anatexis of the Lewisian gneiss. These primary mantle melts have close affinities to Mid-Oceanic Ridge Basalts (MORB), whose trace element content varies from slightly depleted to slightly enriched. Crustal anatexis is a common process in the rift-to-drift evolution during continental break-up and the formation of Volcanic Rifted Margins systems. The ‘early felsic–later mafic’ volcanic rock associations from Rum are compared to similar associations recovered from the now-drowned seaward-dipping wedges on the shelf of SE Greenland and on the Vøring Plateau (Norwegian Sea). These three regions show geochemical differences that result from variations in the regional crustal composition and the depth at which crustal anatexis took place.

Keywords

North Atlantic Igneous ProvinceIsle of RumVøring MarginVolcanic Rifted Marginscrustal contaminationcrustal anatexispetrogenesis
Type
Original Article
Information
Geological Magazine , Volume 146 , Issue 3 , May 2009 , pp. 382 - 399
Copyright
Copyright © Cambridge University Press 2009

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Footnotes

§

Department of Earth Sciences, Uppsala Universitet, Villavägen 16, SE-752 36 Uppsala, Sweden

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