| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.956428 |
| 003 | CaOODSP |
| 005 | 20251031142449 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 251017t20152015oncdab ob f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-on |
| 086 | 1 |aM183-2/7757E-PDF |
| 100 | 1 |aTuba, G., |eauthor. |
| 245 | 10|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 |
| 490 | 1 |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. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v7757.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s14.30 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-7757-eng.pdf |