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Abstract In this paper we present the results of 3D conductive thermal modeling of the Alpine–Pannonian transition zone. The study area comprises the Vienna, Danube, Styrian and Mura–Zala basins, surrounded by the Eastern Alps, the Western Carpathians and Transdanubian Range. The model consists...
Abstract Several explanations have been proposed for variation in geophysical properties and depths for the lithosphere–asthenosphere boundary (LAB) and mid-lithospheric discontinuities (MLD). Here, we investigate the proposal that the dehydration solidus of pargasitic amphibole-bearing upper...
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