Results 121 to 130 of about 416 (175)

Present-day Earth mantle structure set up by crustal pollution of the basal magma ocean. [PDF]

Sci Adv
Ballmer MD, Spaargaren RJ, Mallik A, Manjón-Cabeza Córdoba A, Nakajima M, Vilella K.   +5 more
europepmc   +1 more source

Magnetostratigraphic resolution of the late Ediacaran paleomagnetic enigma

Pierce J, Evans D, Polomski D, Youbi N, Mediany M, Ounar J, Oukhro R, Boumehdi MA, Strauss J, Keller CB, Gärtner A, Ovtcharova M, Wotzlaw J, Linnemann U.   +13 more
europepmc   +1 more source

Nanoscale imaging of Fe-rich inclusions in single-crystal zircon using X-ray ptycho-tomography. [PDF]

Sci Rep
Kuppili VSC, Ball M, Batey D, Dodds K, Cipiccia S, Wanelik K, Fu R, Rau C, Harrison RJ.   +8 more
europepmc   +1 more source

Pseudo-Spectral Modeling in Geodynamo.

, 2007
Reshetnyak, M., Steffen, B.
openaire   +1 more source

Increased and varied radiation during the Sun's encounters with cold clouds in the last 10 million years. [PDF]

Sci Rep
Opher M, Giacalone J, Loeb A, Economo EP, Cummings A, Middleton J, Zucker C, Miller JA, Nica A, Hatzaki M.   +9 more
europepmc   +1 more source

Forecasting secular variation using physics-informed neural networks for IGRF-14. [PDF]

Earth Planets Space
Shakespeare-Rees N, Livermore PW, Davies CJ, Rogers HF, Beggan CD, Brown WJ, Finlay CC.   +6 more
europepmc   +1 more source

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Probing the Geodynamo

Scientific American, 2005
Peter Olson
exaly   +3 more sources

EFFECT OF STRONG EARTHQUAKES ON THE GEODYNAMO

Доклады Российской академии наук. Науки о Земле, 2023
Using the data of magnetic observations performed at the INTERMAGNET network observatories during the period of the double earthquake on March 16, 2022 (Japan), the global nature of the induced geomagnetic variations was demonstrated. Their synchronism and comparable amplitude over a wide range of distances from 210 km to ~10 000 km, the delay time ...
V. V. Adushkin, A. A. Spivak
openaire   +1 more source

Paleomagnetism and the Nature of the Geodynamo

Science, 1990
Records of direct observations of the earth's magnetic field cover less than a ten-millionth of the known lifetime of the field. Thus our knowledge of several geomagnetic phenomena, critical to our understanding of the geodynamo, must come from the paleomagnetic record.
R T, Merrill, P L, McFadden
openaire   +2 more sources