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008260121t20152015oncab   ob   f|0| 0 eng d
040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn-qu
0861 |aM183-2/7911E-PDF
1001 |aBrake, V. I., |eauthor.
24510|aAdditional insights on fracture patterns in the northern Anticosti Basin from satellite, aerial and bathymetric images / |cV. Brake and N. Pinet.
264 1|a[Ottawa] : |bGeological Survey of Canada, |c2015.
264 4|c©2015
300 |a1 online resource (19 pages) : |billustrations, maps.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aOpen file, |x2816-7155 ; |v7911
504 |aIncludes bibliographical references (pages 17-19).
520 |a"Fractures are pervasive across the nearly flat-lying strata of the autochthonous St. Lawrence Platform of the Anticosti Basin. Satellite imagery of the eastern Mingan islands and eastern Anticosti Island exhibit a principal fracture set trending -N105 that is often intersected orthogonally by a -N15 trending fracture set, in agreement with field observations. Lineaments observed on aerial images however are inconsistent with the fractures observed on satellite imagery and are considered a poor reflection of the fracture pattern"--Abstract, page 1.
650 0|aHydraulic fracturing|zQuébec (Province)
650 0|aGeological mapping|zQuébec (Province)
650 6|aFracturation hydraulique|zQuébec (Province)
650 6|aCartographie géologique|zQuébec (Province)
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aOpen file (Geological Survey of Canada)|v7911.|w(CaOODSP)9.506878
85640|qPDF|s2.02 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-7911-eng.pdf
8564 |qHTML|sN/A|uhttps://doi.org/10.4095/296858