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008251017t20152015oncdab  ob   f|0| 0 eng d
040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn-on
0861 |aM183-2/7757E-PDF
1001 |aTuba, G., |eauthor.
24510|aTrace element signature of hydrothermal alteration assemblages (epidote, allanite, actinolite, titanite) in the footwall of the Sudbury Igneous Complex : |ba laser ablation ICP-MS trace element vectoring and fertility study / |cG. Tuba and D.E. Ames.
264 1|a[Ottawa] : |bGeological Survey of Canada, |c2015.
264 4|c©2015
300 |a1 online resource (ii, 29 pages) : |bcharts, illustrations, maps.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aOpen file, |x2816-7155 ; |v7757
504 |aIncludes bibliographical references (pages 27-29).
520 |a"Proper classification is important for guiding future exploration for the low-sulphide metal-rich deposits in the footwall to the Sudbury Igneous Complex. The aim of the study was to establish typical element-associations and behaviours for the paragenetically different hydrothermal assemblages produced during the diverse post-impact magmatic-hydrothermal history of the footwall and hanging-wall units along the North and East ranges of the Sudbury structure to potentially detect a unique signature for alteration related to the high-tenor PGE mineralization"--Abstract, page 1.
650 0|aIgneous rocks|zOntario|zSudbury Structure.
650 6|aRoches ignées|zOntario|zStructure de Sudbury.
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v7757.|w(CaOODSP)9.506878
85640|qPDF|s14.30 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-7757-eng.pdf