| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.895127 |
| 003 | CaOODSP |
| 005 | 20251031142448 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 210108t20202020oncd ob f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-on|an-cn-qu|an-cn-nu |
| 086 | 1 |aM183-2/8706E-PDF |
| 100 | 1 |aPinet, N., |eauthor. |
| 245 | 14|aThe ups and downs of the Canadian Shield. |n3, |padditional apatite fission-track analyses from the Musselwhite, Roberto, Meadowbank and Raglan mines, Ontario, Quebec, and Nunavut / |cN. Pinet and K. McDannell. |
| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2020. |
| 264 | 4|c©2020 |
| 300 | |a1 online resource (49 pages) : |bcharts. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aOpen file ; |v8706 |
| 500 | |aThis record only includes the Open File report in PDF; the complete data set with all the files in various formats is available for free download at http://geoscan.nrcan.gc.ca/. |
| 504 | |aIncludes bibliographical references (pages 23-26). |
| 520 | |a"The low-temperature (ca 120-60°C) thermal history of nine samples from four mines was investigated using the apatite fission-track (AFT) method. Analyses correspond to four samples from the Musselwhite mine over a 275 m vertical interval, three from the Roberto mine over a 382 m vertical interval and one sample from both the Meadowbank and Raglan mines. AFT inverse modelling using both HeFTy and QTQt softwares yield concordant results and indicate that a Phanerozoic heating episode was minor (< 20°C) or non-existent over the Musselwhite mine. This contrasts with previous AFT studies that document significant heating (> 20°C) due to sedimentary burial and indicates that the Canadian Shield did not react as a single entity during the last billion years. The thermal history of samples from the Roberto and Meadowbank mines are less constrained due to the lack of ‘high’ (> 120°C) temperature constraints. The sample from the Raglan mine yields the youngest central age among the samples reported in this study"--Abstract. |
| 650 | 0|aShields (Geology)|zCanada. |
| 650 | 0|aFission track dating. |
| 650 | 6|aBoucliers (Géologie)|zCanada. |
| 650 | 6|aDatation|xMéthode des traces de fission. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aOpen file (Geological Survey of Canada)|v8706.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s4.31 MB|uhttps://publications.gc.ca/collections/collection_2021/rncan-nrcan/m183-2/M183-2-8706-eng.pdf|z(Open File report) |
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/321845|z(complete data set) |