Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.

Forty two oriented samples (97 specimens) were obtained from 17<br />sites in metavolcanic rocks from the Caldwell Group of the Appalachians<br />of Southern Québec (longitude: 71u00'-71"30' W, latitude: 46°00'-46"10'N).<br />Th...

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Main Author: M. K. SEGUIN
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1978-06-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4749
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author M. K. SEGUIN
author_facet M. K. SEGUIN
author_sort M. K. SEGUIN
collection DOAJ
description Forty two oriented samples (97 specimens) were obtained from 17<br />sites in metavolcanic rocks from the Caldwell Group of the Appalachians<br />of Southern Québec (longitude: 71u00'-71"30' W, latitude: 46°00'-46"10'N).<br />These metavolcanics of Lower Cambrian age are massive or pillowed lavas<br />of andesitic and mainly basaltic composition metamorphosed to the<br />sub-greenschist facies. Magnetite and occasionally hematite are the frequent<br />magnetic memory carrier.<br />In order to obtain some pertinent information relative to the stability<br />of the remanent magnetization component, stepwise alternating field<br />demagnetization was conducted on 35% of the specimens and the others<br />were demagnetized at an optimum alternating field. After AF treatment,<br />the paleopole position of the tilted formation from 16 localities is 148°E,<br />43°N (dp=11.3°, dm = 22.4°). After omission of 3 localities for which<br />a95>30°, the new paleopole position obtained is 173°E, 26°N. This formation<br />of Early Cambrian age is characterized by a reversed polarity.
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spelling doaj.art-4412534f35014bf39993ba3920e037932022-12-21T18:51:39ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1978-06-0131119720810.4401/ag-4749Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.M. K. SEGUINForty two oriented samples (97 specimens) were obtained from 17<br />sites in metavolcanic rocks from the Caldwell Group of the Appalachians<br />of Southern Québec (longitude: 71u00'-71"30' W, latitude: 46°00'-46"10'N).<br />These metavolcanics of Lower Cambrian age are massive or pillowed lavas<br />of andesitic and mainly basaltic composition metamorphosed to the<br />sub-greenschist facies. Magnetite and occasionally hematite are the frequent<br />magnetic memory carrier.<br />In order to obtain some pertinent information relative to the stability<br />of the remanent magnetization component, stepwise alternating field<br />demagnetization was conducted on 35% of the specimens and the others<br />were demagnetized at an optimum alternating field. After AF treatment,<br />the paleopole position of the tilted formation from 16 localities is 148°E,<br />43°N (dp=11.3°, dm = 22.4°). After omission of 3 localities for which<br />a95>30°, the new paleopole position obtained is 173°E, 26°N. This formation<br />of Early Cambrian age is characterized by a reversed polarity.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4749
spellingShingle M. K. SEGUIN
Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.
Annals of Geophysics
title Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.
title_full Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.
title_fullStr Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.
title_full_unstemmed Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.
title_short Paleomagnetism of the Caldwell lavas, Eastern Townships, Québec.
title_sort paleomagnetism of the caldwell lavas eastern townships quebec
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4749
work_keys_str_mv AT mkseguin paleomagnetismofthecaldwelllavaseasterntownshipsquebec