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

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Official URL: http://dx.doi.org/10.1038/303492a0

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
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

Item Type:

Publication - Article

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