The nature and timing of deformational events and organic and inorganic metamorphism in the Northern Groundhog Coalfield : implications for the tectonic history of the Bowser Basin
The Groundhog coalfield, located in the northeastern corner of the Bowser Basin of north-central British Columbia, contains approximately a 3700 m thickness of sedimentary rock, ranging in age from Bathonian (Middle Jurassic) to Albian (Early Cretaceous). Four laterally continuous, informal stratigr...
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| Language: | English |
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University of British Columbia
2010
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| Online Access: | http://hdl.handle.net/2429/27145 |