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

Abstract 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...

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Autores principales: Evgeny B. Lebedev, Hartmut Kern, Ninely I. Pavlenkova, Oleg A. Lukanin, Konstantin V. Lobanov, Andrey V. Zharikov, Till Popp
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/810c41d08648421194e6bef0df9b73dc
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