Felsic and mafic magmas in continental crustal settings are derived by melting of the lower
crust and mantle, respectively. This occurs in subduction zone, collisional, extensional and …

At low temperatures (< 750 C at moderate to high crustal pressures), the production of
sufficient melt to reach the melt connectivity transition (∼ 7 vol%), enabling melt drainage …

Abstract Porphyry Cu-(Mo-Au) deposits are relatively rare but reproducible products of
subduction-related magmatism. No unique processes appear to be required for their …

Abstract The Greater India Proterozoic Fold Belt (GIPFOB) is a curved highly tectonized zone
dominated by Early Paleoproterozoic to Early Neoproterozoic magmatic and metamorphic …

Over the last few decades, significant advances in using geophysical techniques to image
the structure of magma plumbing systems have enabled the identification of zones of melt …

The close relationship between crustal magmatism, an expression of heat dissipation, and
tectonics, an expression of stress dissipation, leads to the question of their mutual …

Deciphering the magmatic history of continental magmatic arcs, in general, and the growth
history of individual intrusions, in particular, is key to understanding the complex history of …

Field observations and geophysical data indicate that many igneous bodies grow by
amalgamation of successive magma pulses that commonly take the shape of horizontal …

This paper presents a novel approach to identify complex shapes based on the Radon
transform. We propose an adaptation of Radon transform called R-transform, which is …

The Aeolian volcanoes are located between the Southern Tyrrhenian Sea back arc and the
Calabrian Arc forearc region. Structural, geochemical and seismological data indicate that …