Results 161 to 170 of about 602 (196)
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LITHOSPHERIC MAGNETIC ANOMALIES IN THE BALKAN REGION
2014Bulgarian Geophysical Journal, vol. 40, p.
Abramova, D. +3 more
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International audienceDetailed mapping of Earth’s lithospheric magnetic field provides important insights into the composition, dynamics, and geological history of the crust.
E Thebault, G Hulot
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Magnetic susceptibility anomalies of lithosphere beneath eastern Europe and the Middle East
Geophysics, 1986Abstract Standard inversion methods for inverting aeromagnetic anomalies into magnetic susceptibility contrast in the crust are based on the assumption that the core field is constant over the region considered. This assumption, however, does not hold over regions of a few thousand kilometer extent. An inversion technique is developed
J. Arkani-Hamed, D. W. Strangway
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CHAMP, Ørsted, and Magsat Magnetic Anomalies of the Antarctic Lithosphere
2003We processed CHAMP, Orsted and Magsat mission data for the Antarctic using advanced spectral correlation theory to separate spatially and temporally static components from the dynamic ones. Ignoring measurement noise and processing errors, the dynamic components include strong external field effects, whereas the static components reflect lithospheric ...
Ralph R. B. von Frese +3 more
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The potential contribution to long wavelength magnetic anomalies from the lithospheric mantle
Physics of the Earth and Planetary Interiors, 2019Abstract Long-wavelength magnetic anomalies (LWMA) are broad scale variations of the magnetic field that are usually observed at high altitudes with amplitudes ranging up to about 20 nT. The source of these anomalies has typically been assumed to reside within the crust with negligible contributions from the lithospheric mantle.
Chijioke M. Idoko +3 more
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Journal of Geophysical Research: Solid Earth, 1993
A petromagnetic forward model of induced magnetization of Iceland Plateau is presented. Magnetic susceptibilities of Icelandic rocks from the literature are placed in a vertical stratigraphic context according to a model of igneous and metamorphic layering of the Icelandic crust that is compatible with seismic and other geophysical data. Curie isotherm
Paul B. Toft, Jafar Arkani‐Hamed
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A petromagnetic forward model of induced magnetization of Iceland Plateau is presented. Magnetic susceptibilities of Icelandic rocks from the literature are placed in a vertical stratigraphic context according to a model of igneous and metamorphic layering of the Icelandic crust that is compatible with seismic and other geophysical data. Curie isotherm
Paul B. Toft, Jafar Arkani‐Hamed
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Izvestiya, Physics of the Solid Earth, 2016
For the first time, an attempt is made to apply the data on the lithospheric magnetic anomalies of the Earth for determining the areas prone to strong earthquakes by means of the pattern recognition algorithms. The Caucasian region with the threshold magnitude of the strong earthquakes M0 = 6 is considered.
Alexander A. Soloviev +2 more
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For the first time, an attempt is made to apply the data on the lithospheric magnetic anomalies of the Earth for determining the areas prone to strong earthquakes by means of the pattern recognition algorithms. The Caucasian region with the threshold magnitude of the strong earthquakes M0 = 6 is considered.
Alexander A. Soloviev +2 more
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Long wavelength magnetic anomalies from the lithosphere: Indian shield and Himalaya
Tectonophysics, 1984Abstract A few long-range airborne magnetic profiles flown at an altitude of 7.5 km a.s.l. across the Indian shield are analysed and interpreted in terms of magnetization in the lower crust. The wavelengths of the crustal anomalies are in the range of 51–255 km and this is used to separate them from signals originating at shallow depths.
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Lithospheric Magnetic Anomalies over Large Igneous Province Territories
Izvestiya, Atmospheric and Oceanic Physics, 2022D. Yu. Abramova +3 more
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Exploration Geophysics, 1991
The use of recording magnetometers to observe natural magnetic fluctuations across different parts of Australia is delineating areas where the fluctuations are anomalous. These areas are termed 'conductivity anomalies', as the fluctuation patterns must be due to regions in the lithosphere of high electrical conductivity, where the naturally induced ...
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The use of recording magnetometers to observe natural magnetic fluctuations across different parts of Australia is delineating areas where the fluctuations are anomalous. These areas are termed 'conductivity anomalies', as the fluctuation patterns must be due to regions in the lithosphere of high electrical conductivity, where the naturally induced ...
openaire +1 more source

