Departmental Papers (EES)

Document Type

Journal Article

Date of this Version

April 2001

Abstract

The discovery of a late stage hastingsite gneissic granite in the Inchbae mass (possibly coeval with the riebeckite gneissic granite in the Carn Chuinneag mass) indicates that different physico-chemical conditions prevailed during the last granitic stages of the two masses. This, along with other evidence at the North and SE contacts, is in accord with a previous view that the Inchbae mass is at a different stratigraphic level (lower) relative to the Carn Chuinneag mass.

Comments

Copyright Geological Society. This material has been published in Scottish Journal of Geology Volume 37, Issue 2, 2001, pages 53-57, the only definitive repository of the content that has been certified and accepted after peer review. Copyright and all rights therein are retained by The Geological Society of London.
Publisher URL: http://www.geolsoc.org.uk/template.cfm?name=Journals_JGS_home_page

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Date Posted: 14 October 2005

This document has been peer reviewed.