The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication
The northernmost part of the Cache Creek terrane lies in south-central Yukon and comprises metavolcanic rocks, hemipelagic chert and shale, newly identified volcaniclastic and clastic rocks (Michie formation, informal), pyroxenite and gabbro intrusive rocks with an arc to back-arc geochemical signat...
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crcansciencepubl:10.1139/cjes-2018-0262 2024-03-03T08:49:22+00:00 The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication Bickerton, Luke Colpron, Maurice Gibson, H. Daniel Thorkelson, Derek Crowley, James L. 2020 http://dx.doi.org/10.1139/cjes-2018-0262 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2018-0262 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2018-0262 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 57, issue 2, page 227-248 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 2020 crcansciencepubl https://doi.org/10.1139/cjes-2018-0262 2024-02-07T10:53:31Z The northernmost part of the Cache Creek terrane lies in south-central Yukon and comprises metavolcanic rocks, hemipelagic chert and shale, newly identified volcaniclastic and clastic rocks (Michie formation, informal), pyroxenite and gabbro intrusive rocks with an arc to back-arc geochemical signature, as well as tectonized and serpentinized ultramafic rocks. The proximally sourced Michie formation yielded zircon from two samples with unimodal peaks at 245.85 ± 0.07 and 244.64 ± 0.08 Ma. These dates are likely close to the depositional ages and compare favourably with those from the Kutcho assemblage of northern British Columbia. The Michie formation is exposed along the northwestern flank of Mount Michie and represents singular detrital input from a nearby eroding island-arc. The Cache Creek terrane rocks are imbricated with epiclastic and carbonate rocks of the Stikinia and Lower Jurassic siliciclastic rocks of the synorogenic Whitehorse trough. This imbrication records two compressional deformation phases in the region: (1) an initial phase of west-verging thrusting along the Judas Mountain fault that placed the Cache Creek terrane rocks over the arc and basinal rocks of Stikinia and Whitehorse trough; and (2) a second phase of east-verging thrusting along the Mount Michie fault that repositioned rocks of Stikinia and the Whitehorse trough structurally above those of the Cache Creek terrane. Deformation in the centre of the study area was followed by emplacement of a coarse-grained syenite that yielded 40 Ar/ 39 Ar biotite and muscovite cooling ages of 165–160 Ma. Article in Journal/Newspaper Whitehorse Yukon Canadian Science Publishing Yukon Judas ENVELOPE(-61.116,-61.116,-63.866,-63.866) Judas Mountain ENVELOPE(-134.183,-134.183,60.368,60.368) Mount Michie ENVELOPE(-134.099,-134.099,60.505,60.505) Canadian Journal of Earth Sciences 57 2 227 248 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Bickerton, Luke Colpron, Maurice Gibson, H. Daniel Thorkelson, Derek Crowley, James L. The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication |
topic_facet |
General Earth and Planetary Sciences |
description |
The northernmost part of the Cache Creek terrane lies in south-central Yukon and comprises metavolcanic rocks, hemipelagic chert and shale, newly identified volcaniclastic and clastic rocks (Michie formation, informal), pyroxenite and gabbro intrusive rocks with an arc to back-arc geochemical signature, as well as tectonized and serpentinized ultramafic rocks. The proximally sourced Michie formation yielded zircon from two samples with unimodal peaks at 245.85 ± 0.07 and 244.64 ± 0.08 Ma. These dates are likely close to the depositional ages and compare favourably with those from the Kutcho assemblage of northern British Columbia. The Michie formation is exposed along the northwestern flank of Mount Michie and represents singular detrital input from a nearby eroding island-arc. The Cache Creek terrane rocks are imbricated with epiclastic and carbonate rocks of the Stikinia and Lower Jurassic siliciclastic rocks of the synorogenic Whitehorse trough. This imbrication records two compressional deformation phases in the region: (1) an initial phase of west-verging thrusting along the Judas Mountain fault that placed the Cache Creek terrane rocks over the arc and basinal rocks of Stikinia and Whitehorse trough; and (2) a second phase of east-verging thrusting along the Mount Michie fault that repositioned rocks of Stikinia and the Whitehorse trough structurally above those of the Cache Creek terrane. Deformation in the centre of the study area was followed by emplacement of a coarse-grained syenite that yielded 40 Ar/ 39 Ar biotite and muscovite cooling ages of 165–160 Ma. |
format |
Article in Journal/Newspaper |
author |
Bickerton, Luke Colpron, Maurice Gibson, H. Daniel Thorkelson, Derek Crowley, James L. |
author_facet |
Bickerton, Luke Colpron, Maurice Gibson, H. Daniel Thorkelson, Derek Crowley, James L. |
author_sort |
Bickerton, Luke |
title |
The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication |
title_short |
The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication |
title_full |
The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication |
title_fullStr |
The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication |
title_full_unstemmed |
The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication |
title_sort |
northern termination of the cache creek terrane in yukon: middle triassic arc activity and jurassic–cretaceous structural imbrication |
publisher |
Canadian Science Publishing |
publishDate |
2020 |
url |
http://dx.doi.org/10.1139/cjes-2018-0262 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2018-0262 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2018-0262 |
long_lat |
ENVELOPE(-61.116,-61.116,-63.866,-63.866) ENVELOPE(-134.183,-134.183,60.368,60.368) ENVELOPE(-134.099,-134.099,60.505,60.505) |
geographic |
Yukon Judas Judas Mountain Mount Michie |
geographic_facet |
Yukon Judas Judas Mountain Mount Michie |
genre |
Whitehorse Yukon |
genre_facet |
Whitehorse Yukon |
op_source |
Canadian Journal of Earth Sciences volume 57, issue 2, page 227-248 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/cjes-2018-0262 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
57 |
container_issue |
2 |
container_start_page |
227 |
op_container_end_page |
248 |
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1792506574659387392 |