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040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn---
0861 |aM183-2/8756E-PDF
1001 |aSnyder, D. B., |eauthor.
24510|a3-D mantle structure of the Superior craton / |cD.B. Snyder, A. Vaillancourt, B.A. Kjarsgaard, G. Savard, and E.A. de Kemp.
264 1|a[Ottawa] : |bGeological Survey of Canada, |c2024.
264 4|c©2024
300 |a1 online resource (16 pages) : |bcharts, maps.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aOpen file, |x2816-7155 ; |v8756
504 |aIncludes bibliographical references (pages 13-15).
520 |a"New 3D multi-azimuthal receiver function analysis identified four regional seismic discontinuities dipping at 7–13° within the mantle of the Superior craton of North America; most are discordant to known major upper crustal structures. Widely observed crustal-scale structures with near vertical axial planes striking east-west indicate that the most recent and dominant phase of folding and horizontal shortening strain occurred during the Kenoran (D2) crustal deformation concurrent with Au mineralization and peak metamorphism at 2.72–2.66 Ga. Two mantle discontinuities strike 065° and 249°, dipping to the southeast and northwest, respectively. These strike roughly parallel the northern margin of the Superior craton and some intra-cratonic features such as the axis of the Quetico Basin"--Abstract, page 1.
650 0|aCratons|zCanada.
650 6|aCratons|zCanada.
651 0|aCanadian Shield.
651 6|aBouclier canadien.
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v8756.|w(CaOODSP)9.506878
85640|qPDF|s10.80 MB|uhttps://publications.gc.ca/collections/collection_2024/rncan-nrcan/m183-2/M183-2-8756-eng.pdf
8564 |qHTML|sN/A|uhttps://doi.org/10.4095/p8zz9che61