| 000 | 00000cam 2200000zi 4500 |
| 001 | 9.960673 |
| 003 | CaOODSP |
| 005 | 20260306141028 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 260306t20162016oncdb ob f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-yk |
| 086 | 1 |aM183-2/8170E-PDF |
| 100 | 1 |aMilidragovic, D., |eauthor. |
| 245 | 10|aGeochemistry of Permian rocks of the Yukon-Tanana terrane, western Yukon : |bGEM 2 Cordillera project / |cD. Milidragovic, J.J. Ryan, A. Zagorevski, S.J. Piercey. |
| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2016. |
| 264 | 4|c©2016 |
| 300 | |a1 online resource (21 pages) : |bcharts, maps. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aOpen file ; |v8170 |
| 504 | |aIncludes bibliographical references (page 21). |
| 520 | |a"The geochemical data in this report belong to rocks of the Permian age Klondike assemblage formed during Cycle 6, although some may belong to rocks of the earlier Cycle 5 (Klinkit). Klinkit cycle rocks formed during ca. 314-269 Ma (Pennsylvanian-Early Permian) arc and back-arc volcanism and related sedimentation. Klondike cycle rocks are interpreted to have formed from ca. 265-254 Ma in an arc setting, during westwarddipping subduction of Slide Mountain ocean crust and re-accretion of the Yukon-Tanana terrane to the North American western margin"--Introduction, page 3. |
| 650 | 0|aAnalytical geochemistry|zYukon. |
| 650 | 0|aGeology, Stratigraphic|yPermian. |
| 650 | 6|aGéochimie analytique|zYukon. |
| 650 | 6|aStratigraphie|yPermien. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aOpen file (Geological Survey of Canada)|v8170.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s2.48 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-8170-eng.pdf |
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/299484 |