|
000
| 01952cam 2200337za 4500 |
|---|
| 001 | 9.820696 |
|---|
| 003 | CaOODSP |
|---|
| 005 | 20221107143259 |
|---|
| 007 | cr ||||||||||| |
|---|
| 008 | 160708s2016 oncabd ob f000 0 eng d |
|---|
| 020 | |a978-0-660-04031-8 |
|---|
| 040 | |aCaOODSP|beng |
|---|
| 041 | |aeng|bfre |
|---|
| 043 | |an-cn-yk |
|---|
| 086 | 1 |aM44-2016/1E-PDF |
|---|
| 245 | 00|aGeology and U-Pb geochronology of low-grade mafic rocks from the St. Cyr klippe and a marble from the footwall, Canadian Cordillera, Yukon |h[electronic resource] / |cS.J. Isard ... [et al.]. |
|---|
| 260 | |a[Ottawa] : |bNatural Resources Canada, |c2016. |
|---|
| 300 | |a22 p. : |bcol. charts, col. ill., col. maps. |
|---|
| 490 | 1 |aCurrent research, |x1701-4387 ; |v2016-1 |
|---|
| 504 | |aIncludes bibliographical references. |
|---|
| 520 | |a"This study describes the geological framework for a series of in the northwest part of the St. Cyr area, west of the South Canol Road, in south-central Yukon. The layers of rocks include metamorphic rocks including a higher temperature mafic-ultramafic package and lower temperature packages including phyllite, marble and limestone. Relationships between a number of rock units in the field suggest the rocks were originally formed in an oceanic setting. U-Pb geochronology using zircons confirm the ages for a number of the rock units. These rock units were subsequently faulted into their current location"--Provided by publisher. |
|---|
| 692 | 07|2gccst|aIgneous rocks |
|---|
| 692 | 07|2gccst|aMetamorphic rocks |
|---|
| 692 | 07|2gccst|aGeochronology |
|---|
| 692 | 07|2gccst|aPetrology |
|---|
| 692 | 07|2gccst|aStructural geology |
|---|
| 700 | 1 |aIsard, Sierra J. |
|---|
| 710 | 1 |aCanada. |bNatural Resources Canada. |
|---|
| 710 | 2 |aGeological Survey of Canada. |
|---|
| 830 | #0|aCurrent research (Geological Survey of Canada)|x1701-4387 ; |v2016-1.|w(CaOODSP)9.506236 |
|---|
| 856 | 40|qPDF|s8.95 MB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M44-2016-1-eng.pdf |
|---|