Evidence for a 3.45‐billion‐year‐old magnetic remanence: Hints of an ancient geodynamo from conglomerates of South Africa
- 24 September 2009
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 10 (9)
- https://doi.org/10.1029/2009gc002496
Abstract
No abstract availableKeywords
This publication has 47 references indexed in Scilit:
- Urey ratio and the structure and evolution of Earth's mantleReviews of Geophysics, 2008
- Mantle regulation of core cooling: A geodynamo without core radioactivity?Physics of the Earth and Planetary Interiors, 2007
- Palaeomagnetism of the Neoarchaean Pongola and Ventersdorp Supergroups and an appraisal of the 3.0–1.9Ga apparent polar wander path of the Kaapvaal Craton, Southern AfricaPrecambrian Research, 2007
- Thermal and magnetic evolution of the Earth’s corePhysics of the Earth and Planetary Interiors, 2003
- Estimates of heat flow in the deep mantle based on the power requirements for the geodynamoGeophysical Research Letters, 2002
- Influence of early plate tectonics on the thermal evolution and magnetic field of MarsJournal of Geophysical Research, 2000
- Reassessment of Archean crustal development in the Barberton Mountain Land, South Africa, based on U‐Pb datingTectonics, 1994
- The effect of oxidation on the Verwey transition in magnetiteGeophysical Research Letters, 1993
- Rb‐Sr isotopic systematics of an Archaean granite–gneiss terrain: The Mount Edgar Batholith, Pilbara Block, Western AustraliaAustralian Journal of Earth Sciences, 1990
- Felsic igneous rocks within the 3.3‐ to 3.5‐Ga Barberton Greenstone Belt: High crustal level equivalents of the surrounding Tonalite‐Trondhjemite Terrain, emplaced during thrustingTectonics, 1987