athlete’s-foot
发表于 2025-3-28 15:16:49
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amphibian
发表于 2025-3-28 20:43:40
Book 1991s such as mantle convection, isostasy, and glacial rebound. Yet it remains a poorly resolved parameter and basic questions such as whether the planet‘s response to loading is linear or non-linear, or what are its depth and lateral variations remain uncertain. Part of the answer to such questions lie
palette
发表于 2025-3-28 23:01:26
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Cantankerous
发表于 2025-3-29 06:01:02
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财政
发表于 2025-3-29 08:07:09
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发现
发表于 2025-3-29 15:16:30
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脾气暴躁的人
发表于 2025-3-29 17:40:12
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LINES
发表于 2025-3-29 23:02:36
Luis Bértola,Jeffrey Williamsonhe region when the load is removed, because of the addition of meltwater from the decay of the world’s major ice sheets at about the same time, and because of the rebound occurring from the adjacent Fennoscandian deglaciation. The sea-level observations contain information on the Earth’s rheology as
cumulative
发表于 2025-3-30 01:57:28
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斗争
发表于 2025-3-30 06:48:34
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