Although deep magmatic fluids are important for the shallow magmatic-hydrothermal
evolution and transport/enrichment of ore-forming elements in transcrustal magmatic system …

The Gilów deposit is located in the Góry Sowie Massif of the Central Sudetes (NE Bohemian
Massif, SW Poland). Talcose rocks are associated with serpentinite bodies hosted by …

Mantle volatiles are transported to Earth's crust and surface by basaltic volcanism. During
subaerial eruptions, vast amounts of carbon, sulfur and halogens can be released to the …

Stable sulfur isotope ratios of mid-ocean ridge and ocean island basalts (MORBs and OIBs)
preserve unique information about early Earth processes and the long-term volatile cycles …

Rubidium is a moderately volatile element with high incompatibility and fluid mobility. Its
stable isotopes have great potential in tracing various geological processes. For example …

Outgassing of sulfur (as SO2) is one of the principal hazards posed by volcanic eruptions.
However, S emission potentials of most volcanoes globally are poorly constrained due to a …

Abstract High-silica (SiO 2> 70 wt%) granites in continental collisional zones are crucial for
understanding formation and evolution of the upper continental crust. Fluids released from …

Water significantly impacts the chemical evolution of the Earth's crust, affecting environments
from volcanic settings to hydrothermal systems. These fluids transport elements essential for …

Abstract From September 19 to December 12, 2021, a mixed explosive-effusive eruption
impacted La Palma Island, in the Canary archipelago, leading to the growth of Tajogaite …

Identification of hydrothermal systems affected by magmatic fluid input is relevant for
geothermal energy development. Thus, an approach for identifying such systems based on …