We have analyzed paleointensity data from five polarity transitions and geomagnetic excursions recorded by lava flows. We find a significant correlation between the logarithm of the virtual dipole moment and the angle between the virtual geomagnetic pole and the Earth's rotation axis. This correlation implies that any physical model for geomagnetic field behavior during transitions and excursions must address the question of how changes in direction are linked to changes in intensity. In addition, large changes in paleointensity may occur even when the virtual geomagnetic pole is still at high latitude so the concept of transitional direction must be redefined. <br/
Polarity reversals of the geomagnetic field have occurred through billions of years of Earth history...
Calculations of electromagnetic torques between the fluid outer core and the heterogeneous lower man...
International audienceWe present four new records of the Iceland Basin Excursion (IBE) and five new ...
Geomagnetic polarity transitions are often accompanied by a decrease in magnetic intensity. The time...
Whether Earth's lower mantle observably influences the geodynamo as it attempts to reverse pola...
A previous study of the R3–N3 Icelandic reversal, which corresponds probably to the Matuyama–Réunio...
Earth's magnetic environment is dominated by its mainly dipolar internally generated magnetic field....
Summary. During the Late Tertiary well over 1000 lavas were extruded in Eastern Iceland; potentially...
The paleomagnetic record is central to our understanding of the history of the Earth. The orientatio...
In the context of the dipole model of the earth's magnetic field, the data from the international ba...
Paleomagnetic data on geomagnetic reversals are divided into two general categories: times of occurr...
Centre des Faibles Radioactivit6s, Laboratoire Mixte CNRS-CEA, Gif-sur-Yvette, France Abstract. Most...
International audienceA striking feature of the Steens Mountain (Oregon) geomagnetic polarity revers...
International audienceWe have constructed a very simple model of a time-varying geocentric dipole ba...
copyrighted by American Geophysical UnionWe report the behavior of the earth's magnetic field for a ...
Polarity reversals of the geomagnetic field have occurred through billions of years of Earth history...
Calculations of electromagnetic torques between the fluid outer core and the heterogeneous lower man...
International audienceWe present four new records of the Iceland Basin Excursion (IBE) and five new ...
Geomagnetic polarity transitions are often accompanied by a decrease in magnetic intensity. The time...
Whether Earth's lower mantle observably influences the geodynamo as it attempts to reverse pola...
A previous study of the R3–N3 Icelandic reversal, which corresponds probably to the Matuyama–Réunio...
Earth's magnetic environment is dominated by its mainly dipolar internally generated magnetic field....
Summary. During the Late Tertiary well over 1000 lavas were extruded in Eastern Iceland; potentially...
The paleomagnetic record is central to our understanding of the history of the Earth. The orientatio...
In the context of the dipole model of the earth's magnetic field, the data from the international ba...
Paleomagnetic data on geomagnetic reversals are divided into two general categories: times of occurr...
Centre des Faibles Radioactivit6s, Laboratoire Mixte CNRS-CEA, Gif-sur-Yvette, France Abstract. Most...
International audienceA striking feature of the Steens Mountain (Oregon) geomagnetic polarity revers...
International audienceWe have constructed a very simple model of a time-varying geocentric dipole ba...
copyrighted by American Geophysical UnionWe report the behavior of the earth's magnetic field for a ...
Polarity reversals of the geomagnetic field have occurred through billions of years of Earth history...
Calculations of electromagnetic torques between the fluid outer core and the heterogeneous lower man...
International audienceWe present four new records of the Iceland Basin Excursion (IBE) and five new ...