Sherpa Romeo green journal (pre or post print only)We present a synthesis of paleomagnetic directional data collected from 873 lava flows at 17 different locations under the collaborative Time Averaged geomagnetic Field Initiative (TAFI). The data range from 05 Ma in age, and provide new high quality data with improved spatial coverage. Data quality at each site is measured using k, the best estimate of the Fisherian precision parameter, and its influence on inclination anomaly and VGP dispersion is evaluated by systematically excluding data with successively higher values of k. When combined with regional compilations from NW USA, SW USA, Japan, New Zealand, Hawaii, Mexico, S. Pacific and the Indian Ocean, a data set of 2283 pairs o...
The Fisher distribution is central to palaeomagnetism but presents several problems when used to cha...
This study presents paleomagnetic results from the Snake River Plain (SRP) in southern Idaho as a co...
We review indications of persistent deviations from the geocentric axial dipole model of the time-av...
AbstractInvestigations into long‐term geomagnetic variations provide useful information regarding pa...
Paleomagnetic directions were obtained from stepwise alternating-field or thermal demagnetization of...
The geomagnetic field is predominantly dipolar today, and high-fidelity paleomagnetic mean direction...
The Earth's magnetic field is generally assumed to approximate a geocentric axial dipole (GAD) field...
The current geomagnetic field (GMF) of the Earth is mostly geocentric dipolar with directions on th...
Palaeodirectional data from lava flows and marine sediments provide information about the long-term ...
A volcanic record of geomagnetic field inclination for the past ∼400 kyr at Hilo, Hawaii, has been o...
Palaeodirectional data from lava flows and marine sediments provide information about the long-term ...
Palaeodirectional data from lava flows and marine sediments provide information about the long-term ...
Changes in the Earth's magnetic field have global significance that reach from the outer core extend...
Earth's magnetic environment is dominated by its mainly dipolar internally generated magnetic field....
Earth's magnetic environment is dominated by its mainly dipolar internally generated magnetic field....
The Fisher distribution is central to palaeomagnetism but presents several problems when used to cha...
This study presents paleomagnetic results from the Snake River Plain (SRP) in southern Idaho as a co...
We review indications of persistent deviations from the geocentric axial dipole model of the time-av...
AbstractInvestigations into long‐term geomagnetic variations provide useful information regarding pa...
Paleomagnetic directions were obtained from stepwise alternating-field or thermal demagnetization of...
The geomagnetic field is predominantly dipolar today, and high-fidelity paleomagnetic mean direction...
The Earth's magnetic field is generally assumed to approximate a geocentric axial dipole (GAD) field...
The current geomagnetic field (GMF) of the Earth is mostly geocentric dipolar with directions on th...
Palaeodirectional data from lava flows and marine sediments provide information about the long-term ...
A volcanic record of geomagnetic field inclination for the past ∼400 kyr at Hilo, Hawaii, has been o...
Palaeodirectional data from lava flows and marine sediments provide information about the long-term ...
Palaeodirectional data from lava flows and marine sediments provide information about the long-term ...
Changes in the Earth's magnetic field have global significance that reach from the outer core extend...
Earth's magnetic environment is dominated by its mainly dipolar internally generated magnetic field....
Earth's magnetic environment is dominated by its mainly dipolar internally generated magnetic field....
The Fisher distribution is central to palaeomagnetism but presents several problems when used to cha...
This study presents paleomagnetic results from the Snake River Plain (SRP) in southern Idaho as a co...
We review indications of persistent deviations from the geocentric axial dipole model of the time-av...