Results 91 to 100 of about 2,212 (217)
<p>High-quality relative paleointensity (RPI) is important for the study of Earth Interior and sediments dating. Many existing high-resolution RPI curves have been obtained from the North Atlantic and Pacific Ocean.
Zhou Liang
core +1 more source
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB8601-3
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB8601-
Bleil, Ulrich +3 more
core +1 more source
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 +1 more source
A paleointensity technique for multidomain igneous rocks
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.
Wang, Huapei, Kent, Dennis V.
openaire +4 more sources
The timing of the formation of the Earth's inner core remains a major mystery in the history of Earth's deep interior, with estimates ranging from >1 billion years to
J. Michael Grappone +3 more
doaj +1 more source
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB6007-2
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB6007-
Bleil, Ulrich +3 more
core +1 more source
Paleointensity estimates from oceanic gabbros: Effects of hydrothermal alteration and cooling rate [PDF]
Gabbros recovered by previous ocean drillings were investigated in paleointensity and rock magnetic experiments. The young ages of the samples (ca. 0.78-1.3 Ma) enable a direct comparison between the plutonic paleointensity and volcanic data. Microscopic
Yoichi Usui +4 more
core +1 more source
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 +1 more source
A comparison of different techniques for relative paleointensity
Parallel relative paleointensity records that are supposed to display the same geomagnetic variations often show discrepancies. We compared various techniques of normalization with different parameters involving alternating fields (a.f.) and thermal demagnetization of sediment samples spanning the same period from the Indian and the Pacific oceans. The
Jean‐Pierre Valet, Laure Meynadier
openaire +1 more source
The intensity of the geomagnetic field from 2.4 Ga old Indian dykes
Precambrian paleomagnetic records from dyke swarms provide a unique source of information regarding the Archean geomagnetic field and more specifically the average field strength produced by the early dynamo.
Jean‐Pierre Valet +4 more
doaj +1 more source

