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Secular change of true polar wander over the past billion years

The rate of movement of Earth’s solid shell relative to its spin axis, or true polar wander, depends on variations in mantle convection and viscosity. We report paleomagnetic and geochronologic data from South China that constrain the rate of rapid true polar wander (>5° per million years) betwee...

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Detalles Bibliográficos
Autores principales: Fu, Hairuo, Zhang, Shihong, Condon, Daniel J., Xian, Hanbiao
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9565807/
https://www.ncbi.nlm.nih.gov/pubmed/36240274
http://dx.doi.org/10.1126/sciadv.abo2753