Conclusions a few fundamental relationships are typical to those margins:

  • Rifting task continues for an amazing time frame before breakup and seafloor spreading that is subsequent. For the Nova Scotian margin this era ended up being since great as 40-50 Ma, when it comes to Newfoundland margin 30-40 Ma as well as Labrador 40-65 Ma. Pulses of volcanic task during rifting may possibly occur causing platform uplift due to localized underplating and/or thinning for the lithosphere, however these pulses appear to be localized instead of local in degree. Therefore the margins are predominantly non-volcanic.
  • The spatial degree of main rift task ultimately ultimately causing breakup from the southern margin expands laterally towards the adjacent margin to your north. Therefore the belated Triassic to Early Jurassic rifting regarding the Scotian margin also impacted the Grand Banks together with belated Jurassic to Early Cretaceous rifting in the Grand Banks additionally impacted the Labrador margin.
  • A area of transitional cellar

150 kilometer wide exists seaward regarding the extended continental crust and landward for the first oceanic crust that is normal. This area is related to characteristic alterations in cellar morphology and level throughout the change area, using the deepest, flat-lying cellar in the landward part and elevated cellar highs regarding the side that is seaward. One possibility is the fact that this area is made up primarily of serpentinized mantle with only minor levels of crustal melt (Louden and Chian, 1999). The presence of this change zone is most probably a result of extremely sluggish prices or numerous durations of expansion.

  • Extra refraction that is crustal recently undertaken from the Newfoundland and Scotian margins will assist you to show perhaps the crustal variants previously observed down Labrador are typical to those other margins. Connection of the pages with comparable pages across their margin conjugates may help show whether or not the degree that is high of asymmetry observed when it comes to Labrador-Greenland transect is a very common function associated with the other margin portions. This will suggest whether such asymmetry is really a fundamental results of sluggish prices of lithospheric expansion.
  • It doesn’t matter how many profiles that are seismic models we make, nonetheless, sooner or later we have to drill and core at a couple of areas to find out what exactly is actually here.

    This might be real for cellar goals and for sediment sequences. New drilling that is scientific the Newfoundland basin because of the Ocean Drilling Program if effective will assist you to resolve some fundamental questions regarding its development. But drilling that is additional sequences regarding the slope and rise can also be required to be able to completely understand the type of other major structures. Possibly with a continued mixture of both systematic and commercial tasks, since have actually formerly resulted such an abundance of both knowledge and resources, these future goals may be achieved.


    The Canadian MARIPROBE system is sustained by the Natural Sciences and Engineering analysis Council of Canada. It really is a project that is collaborative Dalhousie University, Memorial University of Newfoundland, University of Calgary while the Geological Survey of Canada. Included in this system, brand brand brand new data that are seismic gathered when you look at the Newfoundland basin through the SCREECH-2000 project associated with Woods Hole Oceanographic organization and also the University of Wyoming, with help through the U.S. Nationwide Science Foundation, along with the Danish Lithosphere Centre.

    About the Author(s)

    Keith Louden is teacher of marine geophysics at Dalhousie University within the Department of Oceanography.

    He stumbled on Dalhousie in 1982, following graduate studies during the Woods Hole Oceanographic Institute and Massachusetts Institute of tech, and research that is post-doctoral Cambridge University. He has got offered as an editor that is associate of Journal of Geophysical Research, Canadian representative on different committees associated with the Ocean Drilling Program (ODP) and also the Global Association of Seismology and Physics regarding the Earth’s Interior (IASPEI), and person in different sub-committees associated with the Lithoprobe Program and CanadaODP. Their research that is current is directed towards studies associated with the framework of rifted continental margins. He’s participated on a lot more than 30 research cruises in many of this world’s oceans. Included in this work, brand brand new instrumentation in seabed seismic recording as well as heat movement have now been created and built at Dalhousie.


    Balkwill, H. R., McMillan, N.J., MacLean, B., Williams, G.L., and Srivastava, S.P., 1990, Geology regarding the Labrador Shelf, Baffin Bay, and Davis Strait: in Geology for the Continental Margin of Eastern Canada, Keen, M.J. And Williams, G.L. (Eds. ), The Geology of United States, Vol. I-1, Geol. Sur. Can., 295-348.

    Bell, J.S. And Campbell, G.R., 1990, Petroleum resources: in Geology for the Continental Margin of Eastern Canada, Keen, M.J. And Williams, G.L. (Eds. ), The Geology of The United States, Vol. I-1, Geol. Sur. Can., 679-719.

    Chian, D., Keen, C. E., Reid, I. And Louden, K.E., 1995, Evolution of non-volcanic margins that are rifted brand brand new outcomes through the conjugate margins of this Labrador water: Geology, 23, 589-592.

    Chian, D., Reid, I.R., and Jackson, H.R., 2001, Crustal framework beneath Orphan Basin and implications for nonvolcanic continental rifting: J. Geophys. Res., 106, 10923-10940.

    Coffin, M. F., Gahagan, L. M., Lawver, L. A., Lee, T. -Y. And Rosencrantz, E., 1992, Atlas of Mesozoic/Cenozoic reconstructions (200 Ma to day that is present: DISHES Progress Report No. 1-0192, Univ. Of Texas Inst. For Geophys., Tech. Rept. No. 122, 49 pp.

    Eldholm, O., Gladczenko, T.P., Skogseid, J., and Planke, S., 2000, Atlantic volcanic margins: a study that is comparative in Dynamics for the Norwegian Margin, Nottvedt, A. Et al. (Eds. ), Geol. Soc. Lond. Spec. Publ., 167, 411-428.

    Enachescu, M.E., 1987, Tectonic and structural framework associated with Northeast Newfoundland continental margin: in Sedimentary Basins and Basin-Forming Mechanisms, Beaumont, C. And Tankard, A.J. (Eds. ), Could. Soc. Pet. Geol., Mem. 12, 117-146.

    Enachescu, M.E., 1992, Enigmatic basins overseas Newfoundland: Can. J. Expl. Geophys., 28, 44-61.

    Gill, R.C.O., Pedersen, A.K. And Larsen, J.G., 1999, Tertiary picrites in western Greenland: melting in the periphery of a plume?: in Magmatism and also the reasons for Continental Break-up, Storey, B.C., Alabaster, T., and Pankhurst, R.J. (Eds. ), Geol. Soc. Lond., 335-348.

    Give, A.C. And McAlpine, K.D., 1990, The margin that is continental Newfoundland: in Geology for the Continental Margin of Eastern Canada, Keen, M.J. And Williams, G.L. (Eds. ), The Geology of United States, Vol. I-1, Geol. Sur. Can., 239-292.

    Hall, J., Louden, K.E., Funck, T., and Deemer, S., 2002, Geophysical faculties regarding the crust that is continental the LITHOPROBE ECSOOT Transect: a review: Can. J. World Sci., in press.