The intrinsic solidification behaviour and glass forming ability (GFA) of natural sub-alkaline
silicate melts have been experimentally quantified via cooling-induced solidification …

Vitreous materials are quite routinely found in natural settings. Most of them are
aluminosilicates, which often occur in large deposits. Considering the geological formations …

New viscosity experiments at superliquidus temperatures and during cooling at a rate of 10
K/hr have been performed at different shear rates on a synthetic pyroxenite melt. Results …

Dynamic cooling-induced solidification experiments were run using six silicate glasses
along the basalt–rhyolite join (B 100= 100 wt.% of basalt, R 100= 100 wt.% of rhyolite), ie B …

High‐temperature experiments were performed in order to shed new light on the shear‐rate
controls on magma viscosity. We compare viscosity data from three different compositions …

Fluorine and chlorine affect phase stabilities in magmatic rocks. We present phase
equilibrium experiments investigating a peralkaline and iron-rich phonolitic composition with …

Historical slags from primary Pb/Ag and Cu smelting can have high contents of valuable
metal (loid) s. So far, there are hardly any studies that provide quantitative information on …

Melt degassing by bubble nucleation and growth is a driving mechanism of magma ascent.
Therefore, decompression experiments with hydrous silicate melts were used to investigate …

Glass stability (GS) indicates the glass reluctance or ability to crystallise upon heating and it
can be characterised by several methods and parameters. GS is frequently used to retrieve …

The viscosity of latitic melts occurring as enclaves in the rhyolitic lava flow of Rocche Rosse
(RR, Lipari, Aeolian Islands, Italy) has been measured in the high T range (1323–1473 K) for …