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The relationship between seismic velocity and density in continental crust - a useful constraint? Stratigraphy, structure and petroleum potential of the Lady Franklin and Maniitsoq Basins, offshore southern West Greenland. Oceanic crustal thickness from seismic measurements and rare Earth element inversion. The only indication of the separately modelled body bas with P -wave velocities of 5. Check yourself for Top 7 common website security bad practices on our Blog Review Threat severity assessment classification Report incorrect detection on helpdesk. At these locations, the acoustic basement is close to the seafloor less than 0. Sediment layers with P -wave velocities ranging from 1. The Ungava Fault Complex is used as a plate boundary; due to the northward motion of Greenland, an overlap of crust needs to be compensated shaded in orange.

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These have formed in the Cretaceous to Eocene during the separation of Greenland from the North American craton e. When the Greenland motion changed to a more northward component, transpressional motion had to be compensated and the Ungava Fault Complex evolved. The thickness is confirmed by OBS 9 Fig. We hiked over rocks identified as the world's oldest, searched for 1,year-old burial sites, and contemplated the fact that before Europeans arrived, the Vikings and two groups of ancestral Inuit lived there. This mantle-derived material gradually intruded the lower crust of the adjacent continental crust and can be related to the Iceland mantle plume. Tectonic evolution of southern Baffin Bay and Davis Strait: Sisimiut looked neat and prosperous. The modelled layers are described in the following paragraphs.

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The complex structure of the basement is incorporated from the high-resolution MCS data Fig. Below the sediment packages sc and sd , we modelled a layer se Fig. Interpretation of the layers are: And it didn't take long to see that even the best-planned expedition couldn't account for nature. We infer that buoyant plume material was channelled southwards along thinned lithosphere in the Davis Strait and formed a zone of magmatic underplating in the northern Labrador Sea. Although rifted margins vary greatly, these global averages fit well to the layers of our model see above. For information on all Lindblad Expeditions-National Geographic cruises, go to www. P -wave velocities of the first crustal layer range from 5.

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With the sun shining, we took off our coats to explore Inuit villages such as Greenland's Sisimiut pop. The average difference between the calculated gravity of the final model Fig. Their mother watched it all, then called them, and the three ambled away.

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