Zircon geochronology reveals polyphase magmatism and crustal anatexis in the Buchan Block, NE Scotland: Implications for the Grampian Orogeny-Reference-Cited by-同舟云学术

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Zircon geochronology reveals polyphase magmatism and crustal anatexis in the Buchan Block, NE Scotland: Implications for the Grampian Orogeny

Published:2017-11 Issue:6 Volume:8 Page:1469-1478
ISSN:1674-9871
Container-title:Geoscience Frontiers
language:en
Short-container-title:Geoscience Frontiers

Author:

Johnson T.E.^ORCID,Kirkland C.L.,Viete D.R.,Fischer S.,Reddy S.M.,Evans N.J.,McDonald B.J.

Funder

Research School of Earth Sciences

Australian National University

AQ44 Australian Education Investment Fund program

ARC LIEF

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference76 articles.

1. Brief thermal pulses during mountain building recorded by Sr diffusion in apatite and multicomponent diffusion in garnet;Ague;Earth and Planetary Science Letters,2007

2. Major shear zones and autochthonous Dalradian in the north-east Scottish Caledonides;Ashcroft;Nature,1984

3. On an intrusion of muscovite-biotite gneiss in the south-eastern highlands of Scotland, and its accompanying metamorphism;Barrow;Quarterly Journal of the Geological Society of London,1893

4. On the geology of Lower Dee-side and the southern Highland Border;Barrow;Proceedings of the Geologists' Association,1912

5. Prograde temperature-time evolution in the Barrovian type-locality constrained by Sm/Nd garnet ages from Glen Clova, Scotland;Baxter;Journal of the Geological Society,2002

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