Geochemistry of the Annidale Group: implications for the tectonic setting of Lower Ordovician volcanism in southwestern New Brunswick
DOI:
https://doi.org/10.4138/2122Abstract
Chemical analyses from volcanic rocks in the Lower Ordovician Annidale Group in southern New Brunswick indicate that it contains two main suites. The volumetrically more abundant suite is bimodal, and consists of within-plate tholeiitic basalt and myolite. The other suite contains rocks that exhibit features indicative of oceanic or possibly subduction-related magmatism. The chemistry of the former suite is consistent with the current interpretation that Ordovician volcanism in southwestern New Brunswick occurred in a back-arc basin. The latter suite, situated near the highly-sheared southeastern margin of the Annidale Group, apparently contains remnants of a different magmatic series near the suture zone between the Gander Zone and the surface expression of the Avalon Zone to the southeast. RÉSUMÉ Les analyses chimiques des roches volcaniques du Groupe d'Annidale, de l'Ordovicien inférieur, dans le sud du Nouvcau-Brunswick indique que celui-ci comprend deux suites principales. La suite la plus abondante en termes de volume est bimodale et comprend des basaltes tholéiitiqucs intraplaques et des rhyolites. L'autre suite contient des roches qui montrent des caractéristiques indiquant un magmatisme océanique ou possiblement relic; a la subduction. La chimie de la première suite est en accord avec l'interprétation prévalant actuellement voulant que le volcanisme ordovicien du sud du Nouveau-Brunswick ait eu lieu dans un bassin d'arrière-arc. La seconde suitée, située près de la bordure sud-est, fortement cisaillée, du Groupe d'Annidale, contient apparemment des reliques d'une séine magmatique différente près de la zone de suture entre la zone de Gander et Pexpression en surface de la zone d'Avalon vers le sud-est. [Traduit par la rédaction]Downloads
Published
How to Cite
Issue
Section
License
All material contained in Atlantic Geology is copyrighted by the journal. Permission to photocopy for internal or personal use or for the internal or personal use of specific clients is granted by Atlantic Geology to libraries and other users registered with the Copyright Clearance Center (CCC), provided that the stated fee per copy is paid directly to the CCC, 21 Congress Street, Salem, Massachusetts 01970 USA. Other requests should be addressed to one of the journal editors, or sent to Atlantic Geology, Box 116, Acadia University, Wolfville, NS, Canada B4P 2R6. Permission to use a single graphic for which Atlantic Geology owns copyright is considered “fair dealing” under the Canadian Copyright Act and “fair use” by the journal, and no other permission need be granted, subject to the image being appropriately cited in all reproductions. The same fair dealing/fair use policy applies to sections of text up to 100 words in length.