On the difficulty of assigning crustal residence, magmatic protolith and metamorphic ages to Lewisian granulites: constraints from combined in situ U–Pb and Lu–Hf isotopes
Author:
Affiliation:
1. Swedish Museum of Natural History and Nordic Center for Earth Evolution (NordCEE), Box 50 007, SE-104 05 Stockholm, Sweden
2. School of Earth and Environmental Sciences, James Cook University, Townsville, Qld 4811, Australia
Abstract
Publisher
Geological Society of London
Subject
Geology,Ocean Engineering,Water Science and Technology
Reference36 articles.
1. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system
2. Lead isotope measurements from the oldest recognised Lewisian gneisses of north-west Scotland
3. Chronology and mechanism of depletion in Lewisian granulites
4. Comment to paper: Timing of magmatism and metamorphism in the Gruinard Bay area of the Lewisian gneiss complex: comparison with the Assynt Terrane and implications for terrane accretion by G.J. Love, P.D. Kinny and C.R.L. Friend (Contr Mineral Petrol (2004) 146:620–636)
5. Polymetamorphic evolution of the Lewisian complex, NW Scotland, as recorded by U-Pb isotopic compositions of zircon, titanite and rutile
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