Results 21 to 30 of about 4,304 (252)
On improving the selection of Thellier-type paleointensity data [PDF]
The selection of paleointensity data is a challenging, but essential step for establishing data reliability. There is, however, no consensus as to how best to quantify paleointensity data and which data selection processes are most effective.
Greig A Paterson, Lisa Tauxe, Ron Shaar
exaly +2 more sources
Archeointensity estimates of a tenth-century kiln: first application of the Tsunakawa–Shaw paleointensity method to archeological relics [PDF]
Paleomagnetic information reconstructed from archeological materials can be utilized to estimate the archeological age of excavated relics, in addition to revealing the geomagnetic secular variation and core dynamics.
Yu Kitahara +5 more
doaj +2 more sources
A paleointensity technique for multidomain igneous rocks [PDF]
We developed a paleointensity technique to account for concave‐up Arai diagrams due to multidomain (MD) contributions to determine unbiased paleointensities for 24 trial samples from site GA‐X in Pleistocene lavas from Floreana Island, Galapagos Archipelago.
Huapei Wang, Dennis V. Kent
openalex +5 more sources
Paleointensity.org is an online, open source, application to analyze paleointensity data produced by the most common paleointensity techniques. Our application currently supports four different methods: thermal Thellier (all variations), microwave ...
Annemarieke Béguin +2 more
exaly +2 more sources
Paleointensity Determination Using the Thellier Technique
The Thellier technique is discussed, specifically in respect of small (3×3mm) samples measured using a cryogenic magnetometer. It is concluded that as long as stringent criteria are imposed the technique gives reliable results. Agreement with the Shaw technique is noted, as also with observatory-based values.
M. J. AITKEN +3 more
openalex +3 more sources
Brunhes Paleomagnetic Directions and Paleointensities From Northern Hainan Island
Paleomagnetic studies typically assume that the long‐term, time‐averaged geomagnetic field behaves as a geocentric axial dipole (GAD). While paleodirectional data over the past five million years generally agree with GAD predictions, mid‐to‐low latitude ...
Mengqing Wang +7 more
doaj +2 more sources
Anisotropy of magnetic remanence (AMR) holds promise for quantifying relative paleointensity values from sedimentary rocks. A proof of concept was established for applied fields that exceeded the intensity of the geomagnetic field.
Felix K. Ostermeier +5 more
doaj +2 more sources
Geomagnetic paleointensity derived from single plagioclase crystals
Rory D Cottrell, John A Tarduno
exaly +2 more sources
Thellier-type paleointensity data from multidomain specimens
Identifying and excluding inaccurate paleointensity estimates that can arise from the effects of multidomain (MD) particles remains a key challenge for paleointensity studies. Here we approach this problem by incorporating realistic experimental noise into a phenomenological MD model, systematically exploring the parameter space of paleointensity ...
Greig A Paterson
exaly +2 more sources
A simple test for the presence of multidomain behavior during paleointensity experiments [PDF]
Greig A Paterson
exaly +2 more sources

