Glacial‐Isostatic Adjustment Models Using Geodynamically Constrained 3D Earth Structures

Abstract Glacial‐isostatic adjustment (GIA) is the key process controlling relative sea‐level (RSL) and paleo‐topography. The viscoelastic response of the solid Earth is controlled by its viscosity structure. Therefore, the appropriate choice of Earth structure for GIA models is still an important a...

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Bibliographic Details
Main Authors: M. Bagge, V. Klemann, B. Steinberger, M. Latinović, M. Thomas
Format: Article
Language:English
Published: Wiley 2021-11-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2021GC009853