Sr, O, and Pb isotope evidence for origin and evolution of Etive Igneous Complex, Scotland
Clayburn, J.A.P.; Harmon, R.S.; Pankhurst, R.J.; Brown, J.F.. 1983 Sr, O, and Pb isotope evidence for origin and evolution of Etive Igneous Complex, Scotland. Nature, 303 (5917). 492-497. https://doi.org/10.1038/303492a0
Full text not available from this repository. (Request a copy)Abstract/Summary
A multi-isotope approach has been applied to the origin of one of the largest and latest Newer Granite complexes of the Scottish Caledonides. Contributions from both mantle and unexposed late Proterozoic lower continental crust are recognized, indicating that granite magmatism is a mechanism for both primary crustal growth and reworking of older crustal rocks.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | https://doi.org/10.1038/303492a0 |
ISSN: | 0028-0836 |
NORA Subject Terms: | Earth Sciences |
Date made live: | 02 Jul 2019 09:16 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/524103 |
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