Results 151 to 160 of about 471 (192)
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New Stochastic Model for Geomagnetic Reversals
Nature, 1970A non-stationary model for geomagnetic reversals is proposed. From the model, a mean length of all polarity intervals of 1.6 m.y. is predicted.
I K, Crain, P L, Crain
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Inhibition and geomagnetic field reversals
Journal of Geophysical Research: Solid Earth, 1993Analysis of the geomagnetic reversal chronology indicates a positive correlation between reversal rate and reversal inhibition. Such a correlation is to be expected between reversal rate and any inhibition resulting from the fact that a reversal transition requires a finite time.
P. L. McFadden, R. T. Merrill
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Nature, 1999
What drives the erratic reversal of Earth's magnetic field? Simulations that allow for variations in heat flow at the core–mantle boundary now implicate events in the mantle. From time to time the Earth's magnetic field reverses in polarity, and the record of such reversals is preserved in rocks magnetized at the time of their formation.
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What drives the erratic reversal of Earth's magnetic field? Simulations that allow for variations in heat flow at the core–mantle boundary now implicate events in the mantle. From time to time the Earth's magnetic field reverses in polarity, and the record of such reversals is preserved in rocks magnetized at the time of their formation.
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Geomagnetic Reversals and Pleistocene Chronology
Nature, 1967The palaeontology and palaeomagnetic stratigraphy of several Atlantic and Pacific cores has been determined to establish the age relationship of various palaeontological boundaries which have been used to define a Pliocene–Pleistocene boundary in deep sea sediments.
B. GLASS +4 more
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