BACKGROUND Volcanoes are surface loci where heat and matter are transferred from the
inner Earth and where the temperatures and pressures of magma, rocks, and fluids change …

To decipher the petrogenesis of chromitites from the Moho Transition Zone of the
Cretaceous Oman ophiolite, we carried out detailed scanning electron microscope and …

Chlorine abundance variations in oceanic basalts can provide insights into the degassing
and volatile recycling history of the mantle as well as shallow melt/hydrosphere interaction …

This work applies a statistical methodology involving the calculation of success rates to
evaluate a total of 28 tectonomagmatic discrimination diagrams: four bivariate (Ti/Y-Zr/Y; Zr …

The Kerguelen Plateau lies in the Southern Indian Ocean and is classically considered as a
Large Igneous Magmatic Province (LIP) emplaced above an oceanic crust. The …

The gravity and bathymetric highs on the Kerguelen Plateau in the southern Indian Ocean
between the Kerguelen Archipelago and Heard Island are seamounts formed of Miocene …

Phase relations of basalts from the Kerguelen large igneous province have been
investigated experimentally to understand the effect of temperature, f O 2, and fugacity of …

After an unusually long quiet period of nearly 6 years, in 1998 the Piton de la Fournaise
volcano started a new cycle of intense volcanic activity. We report geochemical data on the …

High-resolution Fourier transform infrared (FTIR) spectroscopy has been used to document
the presence of hydrogen, to estimate its concentration, and to document its oxygen …

Despite the ubiquity of arsenic in hydrothermal-magmatic environments, its abundance,
distribution, and chemical and structural status in natural silicate melts and glasses remain …