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- W2053237717 abstract "Base metal occurrences in the Carboniferous Windsor Group are commonly associated with carbonate breccias of which three types are recognized: one synsedimentary, one tectonic and one post-burial karstic. The synsedimentary type occurs in the Macumber Formation and in the so-called Pembroke siderite (Walton area); sedimentologic and diagenetic elements indicate rotational slides on a deep-water slope. The tectonic breccia occurs along the top of the Macumbcr Formation and is a manifestation of the Ainslie Detachment, a flat-lying extcnsional fault. Finally, what is referred to as the Pembroke breccia consists of irregularly distributed, post-burial, post-tectonic, post-mineralization, karstic, solution-collapse breccia. The synsedimentary and tectonic breccias are either pre- or syn-ore, although, both have played a key role in localizing mineral deposition through enhanced permeability, as exemplified by the Jubilee and Walton deposits.
 
 RÉSUMÉ
 Les minéralisations métalliferes dans le Groupe de Windsor (Carbonifere) sont généralement associées à des brèches à carbonates desquelles trois types sont reconnues: l'une synsédimentaire, une tectonique et une post-enfouissement karstique. La breche synsédimentaire est présente dans la Formation de Macumber et dans l'unité connue comme la Sidérite de Pembroke (région de Walton); les éléments sédimentologiques et diaginétiques suggèrent des glissements rotation els sur une pente en eau profonde. Une brèche tectonique est présente au sommet de la Formation de Macumber, die est la manifestation du Détachement d'Ainslie, une faille extensionnelle sub-horizontale. Finalement, ce qui est désigné comme la brèche de Pembroke consiste en une brèche karstique d'effondrcment par solution, laquelle est post-enfouissement, post-tectonisme, post-minéralisation et à distribution très iirégulière. Les breches synsédimentaires et tectoniques sont soit pre- ou syn-minéralisation, cependant, ces deux dernières ont joué un rôle crucial dans la localisation des depots minéralises en augmentant la perméabilité des unités, comme illustré par les dépôts de Jubilee et de Walton." @default.
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- W2053237717 date "1995-11-01" @default.
- W2053237717 modified "2023-09-28" @default.
- W2053237717 title "Multiple breccia events in the lower part of the Carboniferous Windsor Group, Nova Scotia" @default.
- W2053237717 doi "https://doi.org/10.4138/2112" @default.
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