Geology, Toad River (northeast), British Columbia / [by] M.E. McMechan. : M183-1/150-2013E-PDF

"The Toad River northeast area (NTS 94-N/NE) in western Liard Basin is underlain by a thick Mississippian to Cretaceous clastic-dominated succession deformed into a few north- or northeast-trending folds. Local abrupt changes in the thickness of Permian sandstone-carbonate and chert units indicate episodes of older block faulting. A major unconformity at the base of the Cretaceous has removed much of the Triassic succession preserved to the southwest. A prominent escarpment capped by Upper Cretaceous Dunvegan conglomerate marks the west limb of the Liard syncline. To the east, poorly exposed Upper Cretaceous conglomerate, shale, and sandstone outline gentle folds. In the Liard Fold and Thrust Belt to the west, four prominent, south-plunging anticlines occur near 60°N. West-directed backthrusts, that follow the locus of older structures and die out southward, offset their steeper west limb at Paleozoic levels. Significant natural gas reserves occur in middle Devonian carbonate beneath the Beaver River Anticline"--Abstract.

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Renseignements sur la publication
Ministère/Organisme Canada. Natural Resources Canada.
Geological Survey of Canada.
Titre Geology, Toad River (northeast), British Columbia / [by] M.E. McMechan.
Titre de la série Canadian geoscience map ; 150
Type de publication Série - Voir l'enregistrement principal
Langue [Anglais]
Format Électronique
Document électronique
Note(s) Includes bibliographical references.
Includes abstract in French.
Information sur la publication Ottawa : Natural Resources Canada, c2013.
Auteur / Contributeur McMechan, Margaret E. (Margaret Evaline), 1953-
Description 1 map : col.
ISBN 978-1-100-22368-1
Numéro de catalogue
  • M183-1/150-2013E-PDF
Numéro de catalogue du ministère 293264
Édition Preliminary version
Données cartographiques Scale 1:100,000
Descripteurs Geological maps
Rivers
Surficial geology
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