Strong temperature gradients associated with slow earthquakes in the mid- and eastern Aleutian Islands revealed by thermal modeling
Published: 5 August 2024| Version 2 | DOI: 10.17632/x65tckk3ms.2
Contributors:
Weiling Zhu, Description
Based on the thermomechanical model Stag3D and the finite difference method (FDM), we constructed a 3D, time-evolving thermomechanical finite difference model. The model dimensions are 1600 km × 750 km × 400 km.
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Institutions
Institute of Tibetan Plateau Research Chinese Academy of Sciences
Categories
Geophysics, Geodynamics