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TitleStratigraphy and structure of the St. Lawrence Lowland in the Charlevoix area, Quebec: relationships to impact cratering
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorLemieux, Y; Tremblay, A; Lavoie, DORCID logo
SourceGeological Survey of Canada, Current Research (Online) no. 2000-D2, 2000, 7 pages, https://doi.org/10.4095/211171 Open Access logo Open Access
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Year2000
PublisherNatural Resources Canada
Documentserial
Lang.English
Mediaon-line; digital; CD-ROM
RelatedThis publication is contained in Current Research 2000
File formatpdf
ProvinceQuebec
NTS21M/08; 21M/09
AreaCharlevoix; St. Lawrence Lowlands
Lat/Long WENS-70.5000 -70.0000 47.7500 47.5000
Subjectstectonics; structural geology; extraterrestrial geology; meteorite craters; craters; faults; rifting; tectonic setting; tectonic evolution; tectonic interpretations; structural interpretations; lithostratigraphy; stratigraphic analyses; unconformities; stratigraphic correlations; shatter cones
Illustrationssketch maps; rose diagrams; photographs
ProgramAppalachian Foreland and St. Lawrence Platform NATMAP Project
Released2000 01 01
AbstractThe Charlevoix area, located 100 km northeast of Quebec City, was the site of a meteoritic impact some 350 million years ago. Few studies have documented the tectonic event sequence of this area before and after the impact. Some field observations suggest that the actual fault systems in the Charlevoix area could have been induced during the rifting of the Iapetan Ocean during Late Proterozoic and Early Cambrian. In addition, those faults could have been reactivated during the meteorite impact and even in Mesozoic time due to rifting of the Atlantic Ocean. However, relationships between the inferred impact cratering with structures left by the Iapetan rifting and/or Mesozoic reactivation have still to be documented.
GEOSCAN ID211171

 
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