| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.959158 |
| 003 | CaOODSP |
| 005 | 20260126091612 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 260121t20152015oncab ob f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-qu |
| 086 | 1 |aM183-2/7911E-PDF |
| 100 | 1 |aBrake, V. I., |eauthor. |
| 245 | 10|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 |
| 490 | 1 |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) |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aOpen file (Geological Survey of Canada)|v7911.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s2.02 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-7911-eng.pdf |
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/296858 |