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Baie Verte area

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Journal Article
Published: 01 March 2001
The Journal of Geology (2001) 109 (2): 191–211.
... = Gander , A = Avalon , C B L = Corner Brook Lake area. Rocks on the Baie Verte Peninsula experienced a complex Ordovican to Silurian structural and metamorphic history. West of the Baie Verte Line, Late Ordovician burial and rapid Silurian exhumation of continental margin...
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The grids of the potential-field data for the <span class="search-highlight">Baie</span> <span class="search-highlight">Verte</span> study <span class="search-highlight">area</span> that we...
Published: 15 June 2021
Figure 2. The grids of the potential-field data for the Baie Verte study area that were sampled to provide the magnetic and gravity data for the SOM-based predictive mapping. (a) TMI (showing areas covered by the three different surveys: 2007 Baie Verte survey top, 1987 Springdale survey
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Geologic map of the study <span class="search-highlight">area</span>, <span class="search-highlight">Baie</span> <span class="search-highlight">Verte</span> Peninsula, with Ming VMS orebodi...
Published: 01 September 2017
Fig. 2. Geologic map of the study area, Baie Verte Peninsula, with Ming VMS orebodies projected to surface (also in the inset) and shown in light red and light green (Lower Footwall zone). Datum is UTM 21N NAD 83. Map compiled and modified from Tuach and Kennedy (1978) , Hibbard (1983
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Generalized geological map of the <span class="search-highlight">Baie</span> <span class="search-highlight">Verte</span> Peninsula showing the position...
Published: 01 March 2001
Figure 1. Generalized geological map of the Baie Verte Peninsula showing the position of the Ming’s Bight Group relative to Humber Zone metaclastic rocks of the Fleur de Lys Supergroup ( FdLS ) and East Pond Metamorphic Suite ( EPMS ) west of the Baie Verte Line, and Dunnage Zone ophiolitic
Journal Article
Published: 01 April 1985
Canadian Journal of Earth Sciences (1985) 22 (4): 607–618.
... Fault. Many of these faults, particularly in the east, are marked by olistostromes, several of which can be dated by fossils as Late Ordovician and Early Silurian. The whole region, between the Reach Fault on the east and the Baie Verte – Brompton Line on the west, has a stratigraphic unity. If it has...
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(A) Early Neoproterozoic paleogeographic reconstruction of Laurentia, Amazo...
Published: 08 March 2022
(modified from Gower, 2019 ). (B) Simplified geologic map of the Baie Verte Peninsula study area (modified from Skulski et al., 2015 ). Striped pattern—outcrop area near Pine Pond. Inset: Newfoundland, showing Humber zone (HZ); Long Range Inlier (LRI); Corner Brook Lake block (CBLB); and Baie Verte
Journal Article
Journal: Geophysics
Published: 15 June 2021
Geophysics (2021) 86 (4): B249–B264.
...Figure 2. The grids of the potential-field data for the Baie Verte study area that were sampled to provide the magnetic and gravity data for the SOM-based predictive mapping. (a) TMI (showing areas covered by the three different surveys: 2007 Baie Verte survey top, 1987 Springdale survey...
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(a) A generalized map of the tectonic divisions of the island of Newfoundla...
Published: 15 June 2021
Figure 1. (a) A generalized map of the tectonic divisions of the island of Newfoundland (modified after Hayes, 2004 ). (b) Simplified geologic map of the Baie Verte Peninsula study area based on the geologic map of Newfoundland by Colman-Sadd et al. (1990) .
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Location map showing the Gaspé Peninsula of southern Quebec, New Brunswick,...
Published: 01 January 2009
Figure 1. Location map showing the Gaspé Peninsula of southern Quebec, New Brunswick, northern Maine and adjacent areas (after Winchester and van Staal, 1994 ). BBL—Baie Verte–Brompton Line; RIL—Red Indian Line.
Journal Article
Published: 07 January 2021
Journal of the Geological Society (2021) 178 (2): jgs2020-093.
...Peter D. Clift; Amy L. Luther; Madison E. Avery; Paul B. O'Sullivan Abstract Early Ordovician collision of the Lough Nafooey Arc (part of the Baie Verte Oceanic Tract) with the passive continental margin of Laurentia peaked at c. 475 Ma in Scotland and Ireland and was followed by subduction...
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Journal Article
Published: 01 February 1978
Canadian Journal of Earth Sciences (1978) 15 (2): 293–300.
...Ian R. Pringle Abstract The Burlington Peninsula, east of the Baie Verte Lineament, is underlain by the Eastern Division of the Fleur de Lys Supergroup, a sequence of metasediments and metavolcanic rocks that is intruded by plutonic masses of granitic to granodioritic composition. This sequence has...
Journal Article
Published: 01 April 1987
Canadian Journal of Earth Sciences (1987) 24 (4): 668–675.
...David B. Scott; Franco S. Medioli; Ann A. L. Miller Abstract Work on new cores from old core sites in Baie Verte, New Brunswick, led to the identification of submerged salt-marsh peats, reported earlier as freshwater ones. A comprehensive sea-level curve, between 9 and 15 m below present, is based...
Journal Article
Journal: Economic Geology
Published: 01 November 1995
Economic Geology (1995) 90 (7): 1955–1965.
... with granodiorite of the Burlington Intrusive Suite, a major regional unit of the eastern Baie Verte... GeoRef, Copyright 2006, American Geological Institute. 1995 ...
Series: GSA Special Papers
Published: 01 January 1993
DOI: 10.1130/SPE275-p85
.... Northwest of the Magog Group, Upper Silurian rocks of the Cranbourne Formation unconformably overlie the Baie Verte-Brompton Line. The Cranbourne Formation is folded and cut by the same regional cleavage as the rocks below the unconformity. This demonstrates that the Acadian Orogeny is the major regional...
Journal Article
Journal: GSA Bulletin
Published: 01 September 1990
GSA Bulletin (1990) 102 (9): 1218–1229.
...ALAIN TREMBLAY; PIERRE ST. JULIEN Abstract Southern Quebec Appalachians Cambro-Ordovician rocks, southeast of the Baie Verte-Brompton Line, belong to the Dunnage Zone and consist of the St. Daniel Mélange, the Ascot Complex, and the Magog Group. The Ascot Complex and the Magog Group are well...
Series: GSA Special Papers
Published: 19 May 2022
DOI: 10.1130/2022.2554(09)
EISBN: 9780813795546
... part of the Baie Verte Peninsula. However, this deformation was localized, because Devonian and Silurian terrestrial sediments in central Newfoundland were generally subjected to little deformation, let alone metamorphism, in many of the areas situated between the Red Indian Line and the Baie Verte...
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