Author:
Kempster R. M. F.,Clarke D. B.,Reynolds P. H.,Chatterjee A. K.
Abstract
Hornblende-rich lamprophyric dykes from southeastern Nova Scotia are contemporaneous with the large peraluminous granitic batholiths (ca. 370 Ma) of the Meguma Zone and may be closely associated with their origin.
Publisher
Canadian Science Publishing
Subject
General Earth and Planetary Sciences
Cited by
31 articles.
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