|
000
| 01859cam 2200349za 4500 |
|---|
| 001 | 9.834623 |
|---|
| 003 | CaOODSP |
|---|
| 005 | 20221107150458 |
|---|
| 007 | cr ||||||||||| |
|---|
| 008 | 170331s2013 oncba #o f000 0 eng d |
|---|
| 040 | |aCaOODSP|beng |
|---|
| 043 | |an-cn--- |
|---|
| 086 | 1 |aM41-11/22-2013E-PDF |
|---|
| 100 | 1 |aKeen, C.E. |
|---|
| 245 | 14|aThe volcanic margins of the northern Labrador Sea |h[electronic resource] / |cC.E. Keen, K. Dickie, and S.A. Dehler. |
|---|
| 260 | |a[Ottawa] : |bNatural Resources Canada, |cc2013. |
|---|
| 300 | |a1 poster : |bill, map. |
|---|
| 490 | 1 |aGeological Survey of Canada, scientific presentation ; |v22 |
|---|
| 500 | |aCaption title. |
|---|
| 500 | |a"Presented at the Third Conjugate Margins Conference. Date presented: August 2012." |
|---|
| 504 | |aIncludes bibliographical references. |
|---|
| 520 | |a“A new interpretation of seismic reflection data on the northern Labrador rifted margin (Keen et al., 2012) shows features which are commonly observed in the igneous crust at volcanic margins, including seaward dipping reflections (SDR), volcanic plateaus, and lava deltas. Below the SDRs, wide angle seismic and gravity data suggest the presence of a thick (~15 km) igneous crust. Comparisons with the well-imaged conjugate west Greenland margin show similar structures there (e.g. Gerlings et al., 2009)"--Introduction. |
|---|
| 692 | 07|2gccst|aVolcanoes |
|---|
| 692 | 07|2gccst|aGeology |
|---|
| 692 | 07|2gccst|aOcean floor |
|---|
| 700 | 1 |aDickie, K. |
|---|
| 700 | 1 |aDehler, S.A. |
|---|
| 710 | 1 |aCanada. |bNatural Resources Canada. |
|---|
| 710 | 2 |aGeological Survey of Canada. |
|---|
| 711 | 2 |aConjugate Margins Conference|n(3rd :|dAugust 2012) |
|---|
| 830 | #0|aScientific presentation (Geological Survey of Canada)|v22|w(CaOODSP)9.820265 |
|---|
| 856 | 40|qPDF|s7.15 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M41-11-22-2013-eng.pdf |
|---|