Results 21 to 30 of about 222,738 (95)
The analysis of the magnetic record of burnt archeological materials provides valuable information of both chronological and geophysical interest. Archeomagnetic studies carried out on independently well-dated materials allow to obtain data in order to ...
Herrejón Lagunilla, Ángela +2 more
core +1 more source
The Politics of Dating Apps [PDF]
An examination of dating app culture in China, across user demographics—straight women, straight men, queer women, and queer men. In this exploration of dating app culture in China, Lik Sam Chan argues that these popular mobile apps are not merely a ...
Chan, Lik Sam
core +1 more source
Reconstruction of Core‐Surface Flows During the Last 3,300 Years
Abstract Understanding the Earth's magnetic field evolution requires examining the fluid flow at the core‐mantle boundary that drives the changes over different timescales. The inversion process to derive core‐surface flow velocities from secular variation data encounters non‐uniqueness issues, necessitating a priori assumptions that yield different ...
Pablo Rivera +2 more
wiley +1 more source
Abstract The study of variations in geomagnetic field intensity over time and space is crucial to understand the evolution of the geodynamo and its interactions with the Earth's surface. In this work, we introduce the SAGEOMAG (South America GEOMAGnetic) database, a comprehensive and updated repository of geomagnetic field intensity records derived ...
Victor J. O. Marum +6 more
wiley +1 more source
Bayesian Inference of Local Paleosecular Variation From Sparse Paleomagnetic Data
Abstract We introduce a novel Bayesian method to construct local paleosecular variation (PSV) curves. By modeling the geomagnetic field as a Gaussian process, global models can be incorporated as informative prior distributions. Because we use Hamiltonian Monte‐Carlo methods, complex age distributions resulting for example from radiocarbon calibration ...
M. A. Schanner, R. Meyer, L. V. de Groot
wiley +1 more source
Brunhes Paleomagnetic Directions and Paleointensities From Northern Hainan Island
Abstract 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 paleointensity records fail to show GAD, with high values from Hawaii.
Mengqing Wang +7 more
wiley +1 more source
Cooling Rate Correction in Paleointensity Experiments on Archeological and Geological Materials
Abstract Obtaining accurate estimates of the absolute intensity of the past geomagnetic field (paleointensity) is one of the major challenges in paleomagnetic research. Paleointensity data are typically determined by replacing the ancient thermoremanent magnetization (TRM) acquired in an unknown field with a laboratory TRM acquired under controlled ...
Ron Shaar
wiley +1 more source
Abstract Correlation of ignimbrite units at polygenic calderas is mandatory for the reconstruction of caldera‐forming events and proper identification of their eruption dynamics. However, ignimbrites erupted at different times from the same caldera can display similarities in composition and lithology that can hamper proper correlation of outcrops ...
Arianna Beatrice Malaguti +5 more
wiley +1 more source
Abstract Grotta Romanelli, located in southern Italy, is a natural coastal cave renowned for its exceptional stratigraphical record and its critical role in understanding the Middle Pleistocene‐Holocene geomorphological and paleoenvironmental evolution of the Mediterranean region.
E. Tema +5 more
wiley +1 more source
Assessing the Reliability of the Pseudo‐Thellier Estimates in Fired Ceramics and Source Clays
Abstract The geomagnetic field's intensity is key to understanding the Earth's core dynamics and their surface impacts. While the Thellier–Thellier method remains the standard for recovering absolute paleointensity from baked materials, it is time‐consuming and may alter magnetic mineralogy due to heating cycles. The pseudo‐Thellier method offers a non‐
Wilbor Poletti +7 more
wiley +1 more source

