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Science Rendezvous > Posters EMAG2: A 2-arc-minute resolution Earth Magnetic Anomaly Grid compiled from satellite, airborne and marine magnetic measurements Maus, S.(1,2), U. Barckhausen (3), H. Berkenbosch (4), N. Bournas (5), J. Brozena (6) ,V. Childers (7), F. Dostaler (8), J. D. Fairhead (9), C. Finn (10), R. R. B. von Frese (11), C. Gaina (12), S. Golynsky (13), R. Kucks (10), H. Lühr (14), P. Milligan ( (1) CIRES, (2) NOAA NGDC, (3) Federal Institute of Geosciences, Germany, (4)Institute of Geological & Nuclear Sciences, New Zealand, (5) Geotech Ltd, Aurora, Canada, (6}{Naval Research Laboratory, USA, (7) NOAA NGS, (8)Geological Survey of Canada, (9}GETE A global Earth Magnetic Anomaly Grid (EMAG2) has been compiled from satellite, ship and airborne magnetic measurements. EMAG2 is specified as a global 2-arc-minute resolution grid of the anomaly of the magnetic intensity at an altitude of 4 km above mean sea level. Magnetic anomaly maps provide insight into the subsurface structure and composition of the Earth's crust. Anomalies trending parallel to the isochrons (lines of equal age) in the oceans reveal the temporal evolution of oceanic crust. Magnetic maps are widely used in the geological sciences and in resource exploration. Furthermore, the global magnetic map is useful in science education to illustrate various aspects of Earth evolution such as plate tectonics and crustal interaction with the deep mantle. Distinct patterns and magnetic signatures can be attributed to the formation (seafloor spreading) and destruction (subduction zones) of oceanic crust, the formation of continental crust by accretion of various terranes to cratonic areas and large scale volcanism (both on continents and oceans). EMAG2 is available at http://geomag.org/models/EMAG2. |
