The geophysical detection of the western EEP boundary at crustal depths, south of the junction with the Carpathian Mts, represents an important geotectonic information when improving regional crustal models. Such geophysical and tectonic models are of great value in SE Europe, where the Vrancea seismo...
setMapData(map,[1 10],eye(20),"grid"); show(map); Find nearest boundary for each corner cell of map. queryIJ = [1 1; 20 1; 1 40; 20 40]; nearestCornerIJ = closestBoundary(map,queryIJ,"grid") nearestCornerIJ = nearestCornerIJ(:,:,1) = 1 6 16 20 nearestCornerIJ(:,:,2...
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Post-orogenic calc-alkaline lamprophyres are relatively abundant in the Variscan Orogen of western and central Europe15,16,28,29,30,31. In addition, at least 30 localities of lamprophyres and closely related igneous rocks are known in southwestern Britain32,33,34,35. The lamprophyres are mica...
if license('test', 'map_toolbox') hold on; coast = load('coast.mat'); plot(coast.long, coast.lat, 'k'); % Plot coastline in black color hold off; else disp('Mapping Toolbox is required to plot the coastline.'); end To d...
RemoveEurope/UzhgorodandEurope/Zaporozhye. Those areas are now covered byEurope/Kyiv. Directly use OpenStreetMap timezone relations for the following zones: Africa/Abidjan Africa/Accra Africa/Addis_Ababa Africa/Algiers Africa/Asmara Africa/Bamako ...
Automotive brands, such as Renault, rely on our platform to bring together hundreds of data points relating to their showrooms and clients across Europe, allowing them to provide accurate insights for network optimization. Category France Boundary Data ...
that sunk down subducting below California. In Oregon and Washington, there’s still a small piece of it that exists which is now called the Juan de Fuca plate. During thetime of Pangaea, the Farallon plate was largely responsible for pulling North America westward away from Europe and Africa...
To create an approximate spatial map of the Levantine spike seen at Earth’s surface we consider the Jordanian and Israeli data to be coeval and centred at 1000 BC. Although there is evidence for two distinct spikes separated by 1–2 centuries in the observations11 we do not make this disti...
However, surface waves with various wavelengths allow us to map gross features of the LAB with a good vertical resolution. We estimate depths to the LAB to be between 200 and 250 km for the Precambrian shields and platforms, around 100 km for the Phanerozoic continental regions and 40–70 ...