Lower-crustal rheology and thermal gradient in the Taiwan orogenic belt illuminated by the 1999 Chi-Chi earthquake

The strength of the lithosphere controls tectonic evolution and seismic cycles, but how rocks deform under stress in their natural settings is usually unclear. We constrain the rheological properties beneath the Taiwan orogenic belt using the stress perturbation following the 1999 Chi-Chi earthquake...

Descripción completa

Detalles Bibliográficos
Autores principales: Tang, Chi-Hsien, Hsu, Ya-Ju, Barbot, Sylvain, Moore, James D. P., Chang, Wu-Lung
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6392777/
https://www.ncbi.nlm.nih.gov/pubmed/30820457
http://dx.doi.org/10.1126/sciadv.aav3287

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6392777/
https://www.ncbi.nlm.nih.gov/pubmed/30820457
http://dx.doi.org/10.1126/sciadv.aav3287

Ejemplares similares