Minutes
发表于 2025-3-23 12:10:34
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maroon
发表于 2025-3-23 17:12:15
Changing ICE Loads on the Earth’s Surface During the Last Glaciation Cyclers, and raised sinusoidally over 20,000 years. Advance and retreat of ice sheets are presented in eleven time steps for North American and Eurasian Ice Sheets, and three time steps for the Antarctic Ice Sheet. Changes over time of total ice volume and ice volume contributing to sea level are compute
刀锋
发表于 2025-3-23 21:51:15
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Fecal-Impaction
发表于 2025-3-24 01:45:37
Secular Sea-Level Changendicating that there is no significant shift in the centre of mass of the ocean relative to the solid Earth. Of the second degree terms only the zonal coefficient is significant with an equatorial sea-level rise and a polar sea-level drop. The contributions from recent changes in mountain glacier vo
Overdose
发表于 2025-3-24 06:18:22
Constraints on Long-Period Sea Level Variations from Global Tide Gauge Data at periods between 2 months and several decades is consistent with the inverted barometer assumption to within about 5%; (d) the global rise in sea level over the last century has been between 1.45 and 2.60 mm/yr, with a preferred value of 1.75 mm/yr; (e) Peltier’s (1986) model for the vertical upl
Reservation
发表于 2025-3-24 10:19:02
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Excitotoxin
发表于 2025-3-24 13:42:29
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立即
发表于 2025-3-24 18:02:32
Chemical Boundaries in the Mantlee high-pressure phases of olivine, β - or γ-spinel. The transition region therefore is olivine-poor, less than about 50% olivine. The properties of the lower mantle are consistent with a “chondritic” Earth, with high FeO and SiO.-contents compared to peridotites. Thus, there is evidence that the sha
彻底明白
发表于 2025-3-24 21:56:28
Book 1991mperature, deformation in geological environments will occur at a much reduced temperature, and thatif at laboratory strain rates a particular deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain
放大
发表于 2025-3-24 23:37:52
1389-2185 ar deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain978-94-010-5492-8978-94-011-3374-6Series ISSN 1389-2185