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The Bathurst Mining Camp
The Bathurst Mining Camp (BMC) occupies a roughly circular area of
approximately 70 km diameter in the Miramichi Highlands of northern New
Brunswick. The area boasts some 46 mineral deposits with defined tonnage
and another hundred mineral occurrences, all hosted by Cambro-Ordovician
rocks that were deposited in an ensialic back-arc basin.
The Bathurst Mining Camp (BMC) virtual field trip contains the following:
- Maps showing the surface distribution of the groups and formations
that comprise the BMC
- Schematic stratigraphic columns of the rock groups
- Digital photos of the rock units* from type-sections and other
significant exposures
- Links to the New Brunswick Stratigraphic Lexicon and to digital
Fieldtrip Guidebooks (see links to PDF files below);
- A listing of Fieldtrip Stops that pertain to corresponding rock
formations/units.
All graphic- and photo-images may be downloaded and used freely.
Questions regarding this virtual field trip or the Bathurst Mining Camp
should be directed to jim.walker@gnb.ca.
*Photo-image descriptions include the NTS Map Sheet and geographic
coordinates (NAD83) of each image’s location.
Maps
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The rocks in the BMC are divided into 5 groups, which are tectonically
as well as lithologically distinct, i.e., they represent 4 major nappes
(themselves internally imbricated) and autocthonous basement rocks that
were juxtaposed by D1 thrusting during closure of the back-arc basin
from the Late Ordovician to Early Silurian. Continued collision between
Gondwana and Laurentia (into the Middle Devonian) produced three further
deformational events (D2, D3, D4) that distorted the rocks of the
BMC into their current complex geometry.
Since the discovery of the No. 6 and No.12 base-metal deposits in
1952 and 1953, the BMC has been the major focus of mineral exploration
in the Province, with expenditures on the order of $225 million (year
2000 dollars) over the past 30 years (Cranstone 2002). |
Approximate outline of Bathurst Mining
Camp
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Interactive Stratigraphy
Field Trip Guidebooks
Related Publications
- Van Staal, C.R., 1994. The Brunswick Subduction Complex in the
Canadian Appalachians: Record of the Late Ordovician to Late Silurian
collision between Laurentia and the Gander Margin of Avalon: Tectonics,
v. 13.
- Van Staal, C.R., 2003. Geology and Tectonic History of the Bathurst
Supergroup, Bathurst Mining Camp, and Its Relationship to Coeval Rocks
in Southwestern New Brunswick and Adjacent Maine – A Synthesis: Economic
Geology, Monograph 11, 2003.
- McCutcheon, S.R., Walker, J.A., and McClenaghan, S.H., 2001. The
Geological Setting of Massive Sulphide Deposits in the Bathurst Mining
Camp: A Synthesis. In Current Research 2000. Edited by B.M.W. Carroll.
New Brunswick Department of Natural Resources and Energy, Mineral
Resource Report 2001-4.
- Cranstone, D. 2002. The discovery and mining of massive
zinc-lead-silver sulphide deposits in New Brunswick – past and future.
In Current Research 2001. Edited by B.M.W. Carroll. New Brunswick
Department of Natural Resources and Energy; Minerals, Policy and
Planning Division, Mineral Resource Report 2002-4, pp.11-40.
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| Last modified:
12/21/2009
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