English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Plus monthly

Global: Zendy Tools annual

Global: Zendy Tools monthly

Global: Zendy Free Plan

The Bateman Brook Metamorphic Suite, as previously defined, is the westernmost unit of the Bras d'Or terrene in the central Cape Breton Highlands. It outcrops along the Eastern Highlands Shear Zone, the contact between the Bras d'Or terrane and the Aspy terrane to the northwest. The Bateman Brook unit has been reported to contain a wide range of lithologies, and contacts with adjacent units are mainly faulted.  Re-examination of rocks from the Bateman Brook Metamorphic Suite shows it to consist of semipelitic to psammitic schist, banded mafic gneiss, and foliated, dioritic, mafic gneiss. Rocks exhibit two major shear fabrics, an early intensely foliated and lineated fabric indicative of shear at high metamorphic grade, and a later mylonitic fabric indicative of shear at lower grade.  As a result of this study, it is recommended that the name Bateman Brook Metamorphic Suite be abandoned. The southern part of the suite is re-assigned to the McMillan Flowage Formation of the Bras d'Or terrane. The central part is interpreted to include rocks of both the Kathy Road Dioritic Suite and the McMillan Flowage Formation. Most of the northern part is re-assigned to the Jumping Brook Metamorphic Suite of the Aspy terrane.  RESUME  La suite metamorphique de Bateman Brook, telle que definie ameiieurement, est l'unite la plus occidentale du terrain de Bras d'Or dans le centre des hautes-terres du Cap-Breton. Elle affleure le long de la zone de cisaillement de Eastern Highlands, le contact entre le terrain de Bras d'Or et le terrain d'Aspy au nord-ouest. L'unite de Bateman Brook a ete decrite comme comprenant une grande variete de lithologies et les contacts avec les unites adjacentes sont principalement failles.  Un reexamen de roches provenant de la suite metamorphique de Bateman Brook montre qu'elle consiste en schiste semi-politique a psammitique, en gneiss mafique rubane et en gneiss mafique dioritique et folie. Les roches montrent deux fabriques de cisaillement majeures, une fabriques de foliation et de lineation precoce fortement developpee indiquant un cisaillement a haut grade metamorphique et une fabrique mylonitique plus tardive indicative d'un cisaillement a plus faible grade.  Comme resultat de cette etude, il est recommande que le terme de suite metamorphique de Bateman Brook soit abandonne La partie sud de la suite est reassignele a la Formation de McMillan Flowage du terrain de Bras d'Or. La partie cent rale est interpretee comme incluant des roches appartenant a la suite dioritique de Kathy Road et a la Formation de McMillan Flowage. La plupart de la partie du nord est reassignee a la suite metamorphique de Jumping Brook du terrain d'Avalon.  [Traduit par la redaction]

A re-interpretation of the "Bateman Brook Metamorphic Suite", Cape Breton Highlands, Nova Scotia, as sheared, fault-bounded blocks of other units