Results 31 to 40 of about 3,470 (247)

Changes in Non‐Dipolar Field Structure Over the Plio‐Pleistocene: New Paleointensity Results From Hawai'i Compared to Global Data Sets

open access: yesJournal of Geophysical Research: Solid Earth, 2023
A foundational assumption in paleomagnetism is that the Earth's magnetic field behaves as a geocentric axial dipole (GAD) when averaged over sufficient timescales.
B. Cych   +4 more
semanticscholar   +1 more source

A Relative Paleointensity (RPI)-Calibrated Age Model for the Corinth Syn-rift Sequence at IODP Hole M0079A (Gulf of Corinth, Greece)

open access: yesFrontiers in Earth Science, 2022
The Corinth basin (Greece) is a young continental rift that recorded cyclic basin paleoenvironment variations (i.e., marine to lacustrine) caused by glacio-eustatic sea level fluctuations during its initial connection to the global oceans.
M. Maffione, E. Herrero-Bervera
semanticscholar   +1 more source

Absolute Paleointensity Experiments on Aged Thermoremanent Magnetization: Assessment of Reliability of the Tsunakawa‐Shaw and Other Methods With Implications for “Fragile” Curvature

open access: yesGeochemistry Geophysics Geosystems, 2022
Absolute paleointensity (API) of the geomagnetic field can be estimated from volcanic rocks by comparing the natural remanent magnetization (NRM) to a laboratory‐induced thermoremanent magnetization (Lab‐TRM).
Y. Yamamoto, L. Tauxe, H. Ahn, C. Santos
semanticscholar   +1 more source

RESET: A Method to Monitor Thermoremanent Alteration in Thellier‐Series Paleointensity Experiments

open access: yesGeophysical Research Letters, 2021
Accurately estimating the paleomagnetic field intensity recorded in terrestrial and planetary materials is the key to understanding dynamo processes. Thellier‐series stepwise‐heating methods with partial thermoremanent magnetization (pTRM) checks for ...
Huapei Wang, D. Kent
semanticscholar   +1 more source

Four‐Dimensional Paleomagnetic Dataset: Plio‐Pleistocene Paleodirection and Paleointensity Results From the Erebus Volcanic Province, Antarctica

open access: yesJournal of Geophysical Research: Solid Earth, 2021
A fundamental assumption in paleomagnetism is that a geocentric axial dipole (GAD) geomagnetic field structure extends to the ancient field. Global paleodirectional compilations that span 0–5‐million year support a GAD dominated field structure with ...
H. Asefaw   +3 more
semanticscholar   +1 more source

Exact Analytical Solutions for Kinetic Equations Describing Thermochemical Remanence Acquisition for Single‐Domain Grains: Implications for Absolute Paleointensity Determinations

open access: yesJournal of Geophysical Research: Solid Earth, 2021
The magnetic record, preserved by igneous rocks in the form of thermoremanent magnetization (TRM) or thermo‐chemical remanent magnetization (TCRM), is essential to reconstruct Earth's absolute paleointensity (API) but strongly depends on the kinetic ...
V. Shcherbakov, F. Lhuillier, N. Sycheva
semanticscholar   +1 more source

Paleointensity database updated [PDF]

open access: yesEos, Transactions American Geophysical Union, 1998
The updated version of the paleointensity database will be included in the new package that should be released by Mike McElhinny in May 1998. The new version comprises 1692 data records from 115 references. The database tables are also available as ASCII and Excel files via an anonymous ftp site (ftp.dstu.
Mereille Perrin   +2 more
openaire   +1 more source

Comparison of Thermal and Microwave Paleointensity Estimates in Specimens Displaying Non‐Ideal Behavior in Thellier‐Style Paleointensity Experiments [PDF]

open access: yes, 2020
Determining the strength of the ancient geomagnetic field is vital to our understanding of the core and geodynamo but obtaining reliable measurements of the paleointensity is fraught with difficulties.
Courtney J. Sprain   +14 more
core   +1 more source

Paleointensities on 8 ka obsidian from Mayor Island, New Zealand [PDF]

open access: yesSolid Earth, 2011
The 8 ka BP (6050 BCE) pantelleritic obsidian flow on Mayor Island, Bay of Plenty, New Zealand, has been investigated using 30 samples from two sites.
A. Ferk   +3 more
doaj   +1 more source

Behavior of paleointensity during the Paleogene [PDF]

open access: yesPhysics of the Earth and Planetary Interiors, 2014
Abstract Behavior of the intensity of geomagnetic field in the Paleogene was studied by the analysis of the sedimentary rocks of the Russian Plate. It is revealed that in the beginning of the Paleogene the variations of little-amplitude paleointensity (about 0.5 H 0 , where H 0 is the value of modern geomagnetic field taken as 40 μT) were ...
A.Yu. Kurazhkovskii   +2 more
openaire   +1 more source

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