Plan and Section, Moose River Gold District, Halifax County, Nova Scotia

1898 ◽  
Author(s):  
E R Faribault
Keyword(s):  
Nova Scotia ◽  
Moose River

Province of Nova Scotia, Halifax County, Moose River Sheet, No 50

1898 ◽  
Author(s):  
E R Faribault
Keyword(s):  
Nova Scotia ◽  
Moose River

scholarly journals Borehole geophysical logs in Meguma gold occurrences, Nova Scotia (Beaver Dam, Moose River and Lake Charlotte areas)

1998 ◽  
Author(s):  
P G Killeen ◽  
B E Elliott ◽  
C N Aoki
Keyword(s):  
Nova Scotia ◽  
Beaver Dam ◽  
Geophysical Logs ◽  
Moose River

Tungsten Deposits of Moose River, Nova Scotia

1910 ◽  
Author(s):  
E R Faribault
Keyword(s):  
Nova Scotia ◽  
Tungsten Deposits ◽  
Moose River

Moose River, Pictou and Guysborough counties, Nova Scotia

1939 ◽  
Author(s):  
Keyword(s):  
Nova Scotia ◽  
Moose River

Paleolatitude and Tectonic Rotations of the Early Carboniferous Fountain Lake Group, Cobequid Highlands, Nova Scotia, Canada

2021 ◽  
Author(s):  
Kate Brooks ◽  
Phil J.A. McCausland ◽  
John W.F. Waldron
Keyword(s):  
Nova Scotia ◽  
Early Carboniferous ◽  
Strike Slip ◽  
Block Rotation ◽  
Beam Analysis ◽  
Recent Origin ◽  
Stable Characteristic ◽  
Dextral Strike Slip ◽  
Slip Motion ◽  
Moose River

The ca. 355 Ma Fountain Lake Group, in the Cobequid Highlands of Nova Scotia, is part of the transtensional basin fill which formed during dextral strike-slip motion between Avalonia and the Meguma terranes following the Acadian Orogeny. Paleomagnetic analysis of the Fountain Lake Group offers a paleolatitude estimate for the Laurentian accretionary margin in the Early Carboniferous and locality-specific paleomagnetic directions which indicate clockwise-sense block rotations during dextral strike-slip motion along the Cobequid Fault zone. Stepwise demagnetization of 142 specimens from 20 sites in three Fountain Lake Group localities across the Cobequid Highlands (Squally Point, West Moose River, and Wentworth exposures) reveals remanence consisting of an easily removed component of probable recent origin, and more persistent components carried by magnetite and hematite, which in petrographic and electron beam analysis appear to be of primary igneous and volcanic oxidation origins, respectively. Sites from all three localities carry stable characteristic remanent magnetization (ChRM) directions that assume similar moderate downward inclinations when tilt-corrected. A Block Rotation Fisher analysis inclination-only fold test demonstrated best agreement at 90% unfolding, showing that remanence acquisition pre-dates Alleghenian deformation in the Late Carboniferous and is most likely of primary 355 Ma age. Paleomagnetic results for the Squally Point, West Moose River and Wentworth localities show relative rotations between the blocks that are variously clockwise-rotated compared with a Laurentia cratonic reference frame. Inclinations at all three localities imply a subtropics paleolatitude for the margin (at Squally Point, 27.2° ± 9.4°; N= 7 sites), directly supporting the depicted location of Laurentia and its Appalachian accretionary margin in most Devonian to Early Carboniferous reconstructions.

Moose River, Pictou and Guysborough counties, Nova Scotia

1939 ◽  
Author(s):  
Keyword(s):  
Nova Scotia ◽  
Moose River

scholarly journals The West Moose River anorthosites, Avalon Zone, Nova Scotia

2002 ◽  
Author(s):  
G Pe-Piper ◽  
G Dessureau
Keyword(s):  
Nova Scotia ◽  
The West ◽  
Moose River

scholarly journals Mineralisation of fractured granites along the Cobequid Fault Zone: West Moose River Pluton, Cumberland County, Nova Scotia

2015 ◽  
Author(s):  
G Pe-Piper ◽  
J Wisen ◽  
A Papoutsa ◽  
D J W Piper
Keyword(s):  
Nova Scotia ◽  
Fault Zone ◽  
Cumberland County ◽  
Moose River

Canada, Nova Scotia, New Brunswick, and the Other British Provinces in North America

2009 ◽  
Author(s):  
James Silk Buckingham
Keyword(s):  
Nova Scotia ◽  
North America ◽  
New Brunswick ◽  
The Other
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