File:Documents de la session de la Puissance du Canada-1912 ( Volume 46, no.19, Documents de la session no.25b-26a) (1912) (14781636484).jpg

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Identifier: documents25b26as1912cana (find matches)
Title: Documents de la session de la Puissance du Canada-1912 ( Volume 46, no.19, Documents de la session no.25b-26a)
Year: 1912 (1910s)
Authors: Canada. Parlement
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Publisher:
Contributing Library: University of Ottawa - Library of Parliament
Digitizing Sponsor: University of Ottawa

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ompo-sant les couches les plus basses de la série palœozoique. Celles-ci se rencontrentdans la partie la plus méridionale de la région et forment une couche plus ou moinsrégulière à la surface des roches anciennes. Le calcaires cristallins de ce districtont généralement une stucture grossière et sont plus ou moins impurs: ils renfermentdes silicates. Les roches groupées sous le nom de gneiss sont, sans doute, toutes dori-gine sédimentaire. Elles représentent parfois des modifications de couches sédimen-taires plus ou moins argileuses, tandis que dautres sont riches en quartz et semblentservir de transition aux quartzites. Associés au gneiss, souvent sans délimitation marquée, se trouvent des schistesbasiques de couleur foncée, groupés par Adam et Barlow sous le nom damphibolites. Ilssont formés de hornblende et de feldspath, et le pyroxène ou la biotite remplacent sou- DEPARTMENT OF MINES MINES BRANCH Magnetqmëtric Map I I I.odynamic lin I I vertical magn. nu EE3
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RAIlOin .VO.l/l/t/A/; 103 DOC. PARLEMENTAIRE No : 6a vent la hornblende en pa^ Quant à leur ori-inc, rcrtaiii^ sent probabh-nicnt des épau-chements oruptifs qui o traversé le calcaire, tandis (;ue dautres sont certainementdorigine sédlmentaire et représentent certaines bandes plus dures et plus ou moinssiliceuses dans les calcair.s primitifs. Txs prranites de cette réj^ion ont une structuregrossière et varient cm . -deur du gris au rouj^eâtrcTls .sont nettement feuilletés bienquà certains en^Vlroi»^ our structure devienn(^ graiiitoïdi- (;t i);i>s< du ^n-anifr typeà un o-neiss granitoiVle. Les syénites onc i ue structure i^rossicre et sont rougeûtre^; elle sont surtout for-mées de feldspath. Elles semblent souvent passer au granité ou au gneiss et il y ades raisons de croire quelles ne sont quune autre forme du nuigma granitique. Les gabbros et diorites ont les caractères dépanchements basiques et ^sont géné-ralement massifs. Comme les granités et les syéni

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Volume
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46
Flickr tags
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  • bookid:documents25b26as1912cana
  • bookyear:1912
  • bookdecade:1910
  • bookcentury:1900
  • bookauthor:Canada__Parlement
  • bookcontributor:University_of_Ottawa___Library_of_Parliament
  • booksponsor:University_of_Ottawa
  • bookleafnumber:1254
  • bookcollection:sessionalpaperscanada
  • bookcollection:universityofottawa
  • bookcollection:toronto
Flickr posted date
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30 July 2014

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