Palaeomagnetic field intensity measurements, derived from rocks with ages that span
geological time, provide a crucial constraint on the evolution of Earth's deep interior and its …

The global paleointensity database for 65–200 Ma was analyzed using a modified suite of
paleointensity quality criteria (QPI) such that the likely reliability of measurements is …

Nearly three decades ago paleomagnetists suggested that there existed a clear link
between latitude dependence of geomagnetic paleosecular variation (PSV) and reversal …

Variations of the Earth's geomagnetic field during the Holocene are important for
understanding centennial to millennial-scale processes of the Earth's deep interior and have …

Many geodynamo models predict an inverse relationship between geomagnetic reversal
frequency and field strength. However, most of the absolute paleointensity data, obtained …

Studying paleosecular variation (PSV) can provide unique insights into the average
morphology of the geomagnetic field and the operation of the geodynamo. Although recent …

We conducted a geomagnetic paleointensity study of lava flows at∼ 30 Ma distributed in the
Lima‐Limo section of the Afro‐Arabian Large Igneous Province. The Tsunakawa‐Shaw …

State-of-the-art measurements of the direction and intensity of Earth's ancient magnetic field
have made important contributions to our understanding of the geology and …

Abstract Knowledge about long-term variation of the geomagnetic dipole field remains in its
nascent stage because of the paucity of reliable experimental data over geological periods …

The geocentric axial dipole (GAD) model is central to many aspects of geophysics, including
plate tectonics and paleoclimate. But its validity is by no means firmly established …