Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians
Deformed terrigenous and carbonate sedimentary rocks representing the early Paleozoic Laurentian continental margin form a series of elongate, fault-bounded blocks that plunge north beneath the Humber Arm Allochthon in the Stephenville area, west Newfoundland Appalachians. The continental shelf succ...
Published in: | Canadian Journal of Earth Sciences |
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Online Access: | http://dx.doi.org/10.1139/e02-041 http://www.nrcresearchpress.com/doi/pdf/10.1139/e02-041 |
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crcansciencepubl:10.1139/e02-041 2024-09-15T18:20:02+00:00 Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians Palmer, Sarah E Waldron, John W.F Skilliter, D M 2002 http://dx.doi.org/10.1139/e02-041 http://www.nrcresearchpress.com/doi/pdf/10.1139/e02-041 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 39, issue 9, page 1393-1410 ISSN 0008-4077 1480-3313 journal-article 2002 crcansciencepubl https://doi.org/10.1139/e02-041 2024-07-25T04:10:06Z Deformed terrigenous and carbonate sedimentary rocks representing the early Paleozoic Laurentian continental margin form a series of elongate, fault-bounded blocks that plunge north beneath the Humber Arm Allochthon in the Stephenville area, west Newfoundland Appalachians. The continental shelf succession was folded and thrust-faulted after emplacement of the Humber Arm Allochthon. In the west of the area, Table Mountain is cut by a "pop-up" structure bounded by downward-converging reverse faults. Structures at the east margin of Table Mountain indicate both dextral and reverse slip. The Phillips Brook Structure, farther east, contains multiple, fault-bounded carbonate slices; one slice, carried by the West Blanche Brook fault, is thrust over the Humber Arm Allochthon. The western edge of the Indian Head massif, consisting of Grenville basement, is also a thrust contact. These reverse faults and thrusts, which cut the carbonate succession and postdate emplacement of the Humber Arm Allochthon, are in turn overprinted by structures formed during dextral strike-slip motion. Unconformable Early Carboniferous cover postdates most of the deformation. Cross-sections indicate shortening of a few kilometres, and basement was clearly involved in the deformation. The Port au Port Peninsula, immediately to the west, records a history of Acadian inversion of Taconian basins. The prevalence of pop-up structures and mappable variations within the stratigraphic units forming the top of the carbonate succession indicate that a complex geometry of Taconian horsts and grabens was inverted during post-Taconian (?Acadian) shortening and dextral strike-slip motion. These relationships suggest a variety of attractive targets in petroleum exploration. Article in Journal/Newspaper Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 39 9 1393 1410 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
language |
English |
description |
Deformed terrigenous and carbonate sedimentary rocks representing the early Paleozoic Laurentian continental margin form a series of elongate, fault-bounded blocks that plunge north beneath the Humber Arm Allochthon in the Stephenville area, west Newfoundland Appalachians. The continental shelf succession was folded and thrust-faulted after emplacement of the Humber Arm Allochthon. In the west of the area, Table Mountain is cut by a "pop-up" structure bounded by downward-converging reverse faults. Structures at the east margin of Table Mountain indicate both dextral and reverse slip. The Phillips Brook Structure, farther east, contains multiple, fault-bounded carbonate slices; one slice, carried by the West Blanche Brook fault, is thrust over the Humber Arm Allochthon. The western edge of the Indian Head massif, consisting of Grenville basement, is also a thrust contact. These reverse faults and thrusts, which cut the carbonate succession and postdate emplacement of the Humber Arm Allochthon, are in turn overprinted by structures formed during dextral strike-slip motion. Unconformable Early Carboniferous cover postdates most of the deformation. Cross-sections indicate shortening of a few kilometres, and basement was clearly involved in the deformation. The Port au Port Peninsula, immediately to the west, records a history of Acadian inversion of Taconian basins. The prevalence of pop-up structures and mappable variations within the stratigraphic units forming the top of the carbonate succession indicate that a complex geometry of Taconian horsts and grabens was inverted during post-Taconian (?Acadian) shortening and dextral strike-slip motion. These relationships suggest a variety of attractive targets in petroleum exploration. |
format |
Article in Journal/Newspaper |
author |
Palmer, Sarah E Waldron, John W.F Skilliter, D M |
spellingShingle |
Palmer, Sarah E Waldron, John W.F Skilliter, D M Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians |
author_facet |
Palmer, Sarah E Waldron, John W.F Skilliter, D M |
author_sort |
Palmer, Sarah E |
title |
Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians |
title_short |
Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians |
title_full |
Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians |
title_fullStr |
Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians |
title_full_unstemmed |
Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians |
title_sort |
post-taconian shortening, inversion and strike slip in the stephenville area, western newfoundland appalachians |
publisher |
Canadian Science Publishing |
publishDate |
2002 |
url |
http://dx.doi.org/10.1139/e02-041 http://www.nrcresearchpress.com/doi/pdf/10.1139/e02-041 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Canadian Journal of Earth Sciences volume 39, issue 9, page 1393-1410 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e02-041 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
39 |
container_issue |
9 |
container_start_page |
1393 |
op_container_end_page |
1410 |
_version_ |
1810458392111611904 |