2000
DOI: 10.1029/1999rg900016
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Geological constraints on the Precambrian history of Earth's rotation and the Moon's orbit

Abstract: Abstract. Over the past decade the analysis of sedimentary cyclic rhythmites of tidal origin, i.e., stacked thin beds or laminae usually of sandstone, siltstone, and mudstone that display periodic variations in thickness reflecting a strong tidal influence on sedimentation, has provided information on Earth's paleorotation and the evolving lunar orbit for Precambrian time (before 540 Ma). Depositional environments of tidal rhythmites range from estuarine to tidal delta, with a wave-protected, distal ebb tidal … Show more

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Cited by 330 publications
(300 citation statements)
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“…Both the mantle and core have evolved since then, including secular cooling, supercontinent aggregation and dispersal, probable nucleation of the solid inner core (Labrosse, 2003), and major reductions in the rate of Earth's rotation due to tidal friction (Williams, 2000). In spite of these evolutionary changes to the core-mantle system, the overall pattern of modulation of geomagnetic reversals persists without any clear indication of a trend.…”
Section: Unresolved Issuesmentioning
confidence: 99%
“…Both the mantle and core have evolved since then, including secular cooling, supercontinent aggregation and dispersal, probable nucleation of the solid inner core (Labrosse, 2003), and major reductions in the rate of Earth's rotation due to tidal friction (Williams, 2000). In spite of these evolutionary changes to the core-mantle system, the overall pattern of modulation of geomagnetic reversals persists without any clear indication of a trend.…”
Section: Unresolved Issuesmentioning
confidence: 99%
“…"According to current measurements in DORIS, GPS, GRACE, VLBI projects, the radius of the Earth in the XXI century has not been changing (the measurement error does not exceed 0.2 mm per year) [11][12][13]. The paleomagnetic and paleogeologic data suggest that the radius of the Earth has not changed significantly over the last 400-600 million years at least" [14,15].…”
Section: Discussionmentioning
confidence: 99%
“…Amongst these was the problem of Earth's rotation. If the Earth's radius were increasing at the fast expansion rate, then the changing moment of inertia of the Earth would have led to significant, observable slowing in the Earth's rotation over the last 200 Ma, well beyond the rate of slowing that has actually been observed (Weijermars, 1986;Williams, 2000). The Earth's density and also its surface gravity would also have been much larger in the Palaeozoic than observations appear to allow.…”
Section: Introductionmentioning
confidence: 95%