|
000
| 01762nam 2200301za 4500 |
|---|
| 001 | 9.819769 |
|---|
| 003 | CaOODSP |
|---|
| 005 | 20230131161136 |
|---|
| 007 | cr ||||||||||| |
|---|
| 008 | 160621s2014 onc|||||o f|0| 0 eng d |
|---|
| 040 | |aCaOODSP|beng |
|---|
| 043 | |an-cn--- |
|---|
| 086 | 1 |aM183-2/7691E-PDF |
|---|
| 100 | 1 |aSnyder, D. B. |
|---|
| 245 | 10|aReport of activities for teleseismic study of Banks Island on the western Arctic margin of the Northwest Territories |h[electronic resource] : |bGEM 2 Western Arctic Margin Project / |c[by] D.B. Snyder. |
|---|
| 260 | |aOttawa : |bNatural Resources Canada, |c2014. |
|---|
| 300 | |a[9] p. : |bmap, figures. |
|---|
| 490 | 1 |aOpen file (Geological Survey of Canada) ; |v7691 |
|---|
| 504 | |aIncludes bibliograhic references. |
|---|
| 520 | |aThis open file report summarizes current understanding of crustal thickness and structure along the western Arctic margin of Canada. The analysis of existing data is inconclusive because of the unusually thin crust(15-24 km)indicated in several locations. The report also describes 2014 repositioning of one teleseismic station in order to increase statistical robustness of results for Banks Island. Crustal and mantle thickness provide important constraints on the geological history with respect to thermal maturation of petroleum source rocks and diamond preservation, respectively. |
|---|
| 692 | 07|2gccst|aSeismology |
|---|
| 692 | 07|2gccst|aEarthquakes |
|---|
| 692 | 07|2gccst|aGeophysics |
|---|
| 692 | 07|2gccst|aGeochemistry |
|---|
| 710 | 1 |aCanada. |bNatural Resources Canada. |
|---|
| 710 | 2 |aGeological Survey of Canada. |
|---|
| 830 | #0|aOpen file (Geological Survey of Canada)|v7691|w(CaOODSP)9.506878 |
|---|
| 856 | 40|qPDF|s579 KB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M183-2-7691-eng.pdf |
|---|