{"id":653,"date":"2013-06-23T21:39:26","date_gmt":"2013-06-23T19:39:26","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-des-anomalies-magnetiques-du-monde\/"},"modified":"2024-04-11T16:35:13","modified_gmt":"2024-04-11T14:35:13","slug":"carte-des-anomalies-magnetiques-du-monde","status":"publish","type":"product","link":"https:\/\/ccgm.org\/en\/product\/world-magnetic-anomalies-map\/","title":{"rendered":"Magnetic Anomaly Map of the World"},"content":{"rendered":"
Magnetic Anomaly Map of the World<\/strong><\/p>\n This map is the first global compilation of the vast amount of data collected over the past 50 years from aeromagnetic surveys of land areas, magnetometry profiles recorded during sea campaigns to assess the age of the oceanic crust, and satellite observations.<\/p>\n The aim of this map is to help interpret surface observations of the Earth's geological composition and structure. Metamorphism, petrology and redox states have major effects on the magnetic state of the minerals that make up the material of the crust.<\/p>\n The magnetic anomalies shown on this map originate from the formation and composition of igneous and metamorphic rocks in the Earth's crust, probably in the upper part of the Earth's mantle, i.e. in the lithosphere.<\/p>\n What we call the magnetic anomaly field corresponds roughly to the lithospheric field, which represents the difference between the measured data, which includes all the magnetic sources, and the estimated core and external fields. This anomalous field is therefore created inside the magnetic lithosphere, but it is important to bear in mind that only structures with an amplitude of less than 2,500 km can be taken into account.<\/p>\n In almost all cases, the magnetic anomaly field represents less than 1% of the total magnetic field.<\/p>\n The study of crustal magnetism has contributed, among other things, to the development of geodynamic models of the lithosphere, geological mapping and natural resource exploration.<\/p>\n Magnetic Anomaly Map of the World<\/strong><\/p>\n Earth magnetism map data such as the one presented here, in conjunction with other information, can be very useful in defining geological provinces, locating impact structures, dykes, faults and other geological formations with magnetic contrasts to their surroundings.<\/p>\n For this reason, the Magnetic Anomaly Map of the World is published in printed and digital form, together with a database on DVD. The magnetic field shown on the map corresponds to an altitude of 5 km above the WGS84 ellipsoid.<\/p>\n