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Fluid-driven low-grade metamorphism in polydeformed rocks of Avalonia (Arisaig Group, Nova Scotia, C...

Fluid-driven low-grade metamorphism in polydeformed rocks of Avalonia (Arisaig Group, Nova Scotia, C...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1458536540

Fluid-driven low-grade metamorphism in polydeformed rocks of Avalonia (Arisaig Group, Nova Scotia, Canada)

About this item

Full title

Fluid-driven low-grade metamorphism in polydeformed rocks of Avalonia (Arisaig Group, Nova Scotia, Canada)

Publisher

Basel: SP Birkhäuser Verlag Basel

Journal title

Swiss Journal of geosciences, 2012-07, Vol.105 (2), p.283-297

Language

English

Formats

Publication information

Publisher

Basel: SP Birkhäuser Verlag Basel

More information

Scope and Contents

Contents

The Lower Silurian—Lower Devonian Arisaig Group (Antigonish Highlands) in the Canadian Appalachians is a sequence of shallow marine strata deposited after the accretion of Avalonia to Baltica during the closure of the Iapetus Ocean. Deformation of the strata is widely attributed to the Devonian Acadian orogeny and produced shallowly plunging region...

Alternative Titles

Full title

Fluid-driven low-grade metamorphism in polydeformed rocks of Avalonia (Arisaig Group, Nova Scotia, Canada)

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_1458536540

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1458536540

Other Identifiers

ISSN

1661-8726

E-ISSN

1661-8734

DOI

10.1007/s00015-012-0096-2

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