FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN
An alternative model for the formation of Devonian carbonate reefs in the Western Canada Basin is proposed. This model is based on the epeiric clear‐water sedimentation model of Irwin (1965), with structural modfication throughout the Phanerozoic by repeated PreCambrian basement tectonism. The crato...
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crwiley:10.1111/j.1747-5457.1989.tb00239.x 2024-03-31T07:52:08+00:00 FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN Greggs, R. G. Greggs, D. H. 1989 http://dx.doi.org/10.1111/j.1747-5457.1989.tb00239.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1747-5457.1989.tb00239.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1747-5457.1989.tb00239.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Petroleum Geology volume 12, issue 4, page 377-404 ISSN 0141-6421 1747-5457 Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology journal-article 1989 crwiley https://doi.org/10.1111/j.1747-5457.1989.tb00239.x 2024-03-04T13:01:56Z An alternative model for the formation of Devonian carbonate reefs in the Western Canada Basin is proposed. This model is based on the epeiric clear‐water sedimentation model of Irwin (1965), with structural modfication throughout the Phanerozoic by repeated PreCambrian basement tectonism. The cratonic structural pattern is dominantly controlled by the global regmatic fracture‐system, which comprises a series of NW ‐ SE and NE ‐ SW vertical faults. These faults delineate a mosaic of fault blocks across the entire Western Canada Basin. Wrench faulting and vertical epeirogenic movements throughout the Paleozoic. Mesozoic, and Cenozoic subjected these blocks to further tectonic effects ‐ structural deformation and hydrothermal diagenesis. Preservation of down‐faulted carbonate blocks, and their subsequent isostatic recovery into overlying anhydrite or shale sequences, has led to the formation of carbonate complexes generally referred to as “organic reefs”. In addition, repeated emergence and submergence of the cratonic platform, particularly throughout the Middle and Upper Paleozoic, produced numerous regional and inter‐regional unconformities. These periods of erosion contributed to the leaching, and partial dolomitization, of the Devonian carbonates formed during periods of cratonic submergence. Repeated faulting is considered to have been a major factor in the diagenetic alteration of Devonian carbonates through associated hydrothermal activity, and a dominant control in the migration of hydrocarbons. Article in Journal/Newspaper canada basin Wiley Online Library Canada Journal of Petroleum Geology 12 4 377 404 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
topic |
Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology |
spellingShingle |
Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology Greggs, R. G. Greggs, D. H. FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN |
topic_facet |
Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology |
description |
An alternative model for the formation of Devonian carbonate reefs in the Western Canada Basin is proposed. This model is based on the epeiric clear‐water sedimentation model of Irwin (1965), with structural modfication throughout the Phanerozoic by repeated PreCambrian basement tectonism. The cratonic structural pattern is dominantly controlled by the global regmatic fracture‐system, which comprises a series of NW ‐ SE and NE ‐ SW vertical faults. These faults delineate a mosaic of fault blocks across the entire Western Canada Basin. Wrench faulting and vertical epeirogenic movements throughout the Paleozoic. Mesozoic, and Cenozoic subjected these blocks to further tectonic effects ‐ structural deformation and hydrothermal diagenesis. Preservation of down‐faulted carbonate blocks, and their subsequent isostatic recovery into overlying anhydrite or shale sequences, has led to the formation of carbonate complexes generally referred to as “organic reefs”. In addition, repeated emergence and submergence of the cratonic platform, particularly throughout the Middle and Upper Paleozoic, produced numerous regional and inter‐regional unconformities. These periods of erosion contributed to the leaching, and partial dolomitization, of the Devonian carbonates formed during periods of cratonic submergence. Repeated faulting is considered to have been a major factor in the diagenetic alteration of Devonian carbonates through associated hydrothermal activity, and a dominant control in the migration of hydrocarbons. |
format |
Article in Journal/Newspaper |
author |
Greggs, R. G. Greggs, D. H. |
author_facet |
Greggs, R. G. Greggs, D. H. |
author_sort |
Greggs, R. G. |
title |
FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN |
title_short |
FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN |
title_full |
FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN |
title_fullStr |
FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN |
title_full_unstemmed |
FAULT‐BLOCK TECTONISM IN THE DEVONIAN SUBSURFACE, WESTERN CANADA BASIN |
title_sort |
fault‐block tectonism in the devonian subsurface, western canada basin |
publisher |
Wiley |
publishDate |
1989 |
url |
http://dx.doi.org/10.1111/j.1747-5457.1989.tb00239.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1747-5457.1989.tb00239.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1747-5457.1989.tb00239.x |
geographic |
Canada |
geographic_facet |
Canada |
genre |
canada basin |
genre_facet |
canada basin |
op_source |
Journal of Petroleum Geology volume 12, issue 4, page 377-404 ISSN 0141-6421 1747-5457 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1747-5457.1989.tb00239.x |
container_title |
Journal of Petroleum Geology |
container_volume |
12 |
container_issue |
4 |
container_start_page |
377 |
op_container_end_page |
404 |
_version_ |
1795031118365327360 |