Compressional wave velocity measurements on mafic–ultramafic rocks under high aqueous fluid pressure and temperature help to explain low-velocity zones in the lithosphere

Deep seismic studies have revealed that low-velocity zones mainly occurred in the continental lithosphere at the depth of 100–150 km. Their origin has not been clearly explained yet. The article demonstrates the possible scale of Vp changes in crystalline rocks of different composition. The conclusi...

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Detalles Bibliográficos
Autores principales: Lebedev, Evgeny B., Kern, Hartmut, Pavlenkova, Ninely I., Lukanin, Oleg A., Lobanov, Konstantin V., Zharikov, Andrey V., Popp, Till
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8239040/
https://www.ncbi.nlm.nih.gov/pubmed/34183696
http://dx.doi.org/10.1038/s41598-021-92248-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8239040/
https://www.ncbi.nlm.nih.gov/pubmed/34183696
http://dx.doi.org/10.1038/s41598-021-92248-2

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