The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny

The Cross Lake Group, consisting of basalt, conglomerate, and sandstone, lies unconformably on the basement biotite granodiorite gneiss. The area probably underwent two periods of folding and these likely correspond to the Kenoran and Hudsonian orogenies. The only recognizable effects of the Kenoran...

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Main Author: Rousell, D. H.
Language:unknown
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/1993/5418
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spelling ftcanadathes:oai:collectionscanada.gc.ca:MWU.1993/5418 2023-05-15T15:55:04+02:00 The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny Rousell, D. H. 2012-05-09T20:18:12Z http://hdl.handle.net/1993/5418 unknown http://hdl.handle.net/1993/5418 2012 ftcanadathes 2014-03-30T00:51:21Z The Cross Lake Group, consisting of basalt, conglomerate, and sandstone, lies unconformably on the basement biotite granodiorite gneiss. The area probably underwent two periods of folding and these likely correspond to the Kenoran and Hudsonian orogenies. The only recognizable effects of the Kenoran orogeny are the north northeasterly and north northwesterly - trending cross folds. The Cross Lake Group was folded, metamorphosed, and granitized during the Hudsonian orogeny. The major structural features were produced during the Hudsonian orogeny. These consist of a southwesterly-trending syncline and a northwesterly-trending syncline which merge and continue as one to the southwest and a major anticline situated between the two arms of the synclines. Numberous small-scales folds and lineations are present. Structures, in general, plunge steeply. Gabbro and anorthosite in the form of a sill at Pipestone Lake and a batholith south of the Minago River intrude the Cross Lake Group. These bodies were emplaced before or during the early stages of the Hudsonian folding. Previous writers suggest that the Churchill and Superior provinces in northern Manitoba are separated by a gneissic zone. This study indicates that the contact between the Cross Lake sedimentary - Volcanic belt ("Superior" province) and the gneissic zone is a gradational one. Rocks south of the contact consist of those of the Cross Lake group and migmatites and rocks north of the contact are migmatites and those of the gneiss complex. Evidence is presented which suggests that the Cross Lake area lies within the Churchill province and that the Churchill-Superior boundary lies south of Cross Lake. The contact is likely a gradational one where effects of the Hudsonian orogeny face into the Superior province. Other/Unknown Material Churchill Theses Canada/Thèses Canada (Library and Archives Canada) Pipestone Lake ENVELOPE(-106.584,-106.584,57.900,57.900)
institution Open Polar
collection Theses Canada/Thèses Canada (Library and Archives Canada)
op_collection_id ftcanadathes
language unknown
description The Cross Lake Group, consisting of basalt, conglomerate, and sandstone, lies unconformably on the basement biotite granodiorite gneiss. The area probably underwent two periods of folding and these likely correspond to the Kenoran and Hudsonian orogenies. The only recognizable effects of the Kenoran orogeny are the north northeasterly and north northwesterly - trending cross folds. The Cross Lake Group was folded, metamorphosed, and granitized during the Hudsonian orogeny. The major structural features were produced during the Hudsonian orogeny. These consist of a southwesterly-trending syncline and a northwesterly-trending syncline which merge and continue as one to the southwest and a major anticline situated between the two arms of the synclines. Numberous small-scales folds and lineations are present. Structures, in general, plunge steeply. Gabbro and anorthosite in the form of a sill at Pipestone Lake and a batholith south of the Minago River intrude the Cross Lake Group. These bodies were emplaced before or during the early stages of the Hudsonian folding. Previous writers suggest that the Churchill and Superior provinces in northern Manitoba are separated by a gneissic zone. This study indicates that the contact between the Cross Lake sedimentary - Volcanic belt ("Superior" province) and the gneissic zone is a gradational one. Rocks south of the contact consist of those of the Cross Lake group and migmatites and rocks north of the contact are migmatites and those of the gneiss complex. Evidence is presented which suggests that the Cross Lake area lies within the Churchill province and that the Churchill-Superior boundary lies south of Cross Lake. The contact is likely a gradational one where effects of the Hudsonian orogeny face into the Superior province.
author Rousell, D. H.
spellingShingle Rousell, D. H.
The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny
author_facet Rousell, D. H.
author_sort Rousell, D. H.
title The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny
title_short The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny
title_full The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny
title_fullStr The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny
title_full_unstemmed The petrology of Archean and Proterozoic rocks at Cross Lake, Manitoba and the effects of the Hudsonian orogeny
title_sort petrology of archean and proterozoic rocks at cross lake, manitoba and the effects of the hudsonian orogeny
publishDate 2012
url http://hdl.handle.net/1993/5418
long_lat ENVELOPE(-106.584,-106.584,57.900,57.900)
geographic Pipestone Lake
geographic_facet Pipestone Lake
genre Churchill
genre_facet Churchill
op_relation http://hdl.handle.net/1993/5418
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