Estimates of the Temperature and Melting Conditions of the Carpathian‐Pannonian Upper Mantle From Volcanism and Seismology

Abstract What drives the formation of basaltic melts beneath intraplate volcanoes not associated with extensive thermal anomalies or lithospheric extension? Detailed constraints on the melting conditions and source region are imperative to resolve this question. Here we model the geochemistry of alk...

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Hlavní autoři:	Antoine J. J. Bracco Gartner, Dan McKenzie
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2020-10-01
Edice:	Geochemistry, Geophysics, Geosystems
Témata:	Carpathian‐Pannonian region intraplate volcanism melt generation rare‐earth element inversion mantle potential temperature asthenospheric upwelling
On-line přístup:	https://doi.org/10.1029/2020GC009334
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