Transient rheology of the Sumatran mantle wedge revealed by a decade of great earthquakes

The rheology of the upper mantle is key to understanding how plate tectonics may evolve. Here, using GPS and tide-gauge measurements along the Sumatran subduction zone, the authors’ show that a bi-viscous rheology model is needed to explain the stress and strain evolution of the upper mantle followi...

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Autores principales: Qiang Qiu, James D. P. Moore, Sylvain Barbot, Lujia Feng, Emma M. Hill
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/23d0070dc57c4a4398890ba45b6a98b2
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