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Updated: Jul 12, 2026

06:29
Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
Published on: February 27, 2021
Volcanic eruptions: contribution to magnetism in deep-sea sediments downwind from the azores
Abstract:
The mean bulk magnetic susceptibility (x) and the intensity of remanent magnetization (J) of deep-sea sediments vary systematically, but in an opposite sense, for a distance of 600 kilometers downwind from the Azores. Beyond the distance both J and x diminish for at least another 600 kilometers. The dominant type of magnetic particle in the sediments is interpreted to be atmospherically transported volcanic dust.
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