Titlebook: Glacial Isostasy, Sea-Level and Mantle Rheology; R. Sabadini,K. Lambeck,E. Boschi Book 1991 Springer Science+Business Media Dordrecht 1991

athlete’s-foot

amphibian

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

Cantankerous

财政

发现

脾气暴躁的人

LINES

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

斗争