Partial melts in the Earth's convecting mantle influence its physical and chemical state,
particularly the plasticity of the asthenosphere and the dynamics of plate tectonics. Melt …

The oceanic-island magmatic systems of the Atlantic Ocean exhibit significant diversity in
their respective sizes, ages, and the compositional ranges of their eruptive products …

The concentration of carbon in primary mid‐ocean ridge basalts (MORBs), and the
associated fluxes of CO2 outgassed at ocean ridges, is examined through new data …

ABSTRACT A synthetic model is presented to enlarge the evolutionary framework of the
General Dynamic Model (GDM) and the Glacial Sensitive Model (GSM) of oceanic island …

Lead (Pb) isotopes provide valuable insights into the origin of Pb within a sample, typically
allowing for reliable fingerprinting of their source. This is useful for a variety of applications …

Lithological heterogeneity is a widely accepted feature of the Earth's mantle, with recycled
crustal material accounting for a significant part of heterogeneity in ocean island basalt (OIB) …

The growth and decay of oceanic volcanoes developed close to plate boundaries are
intrinsically related to a competition between construction and destruction processes, partly …

The Azores region straddles the Mid-Atlantic Ridge and comprises volcanic islands and
seamounts interspersed with non-magmatic oceanic basins arranged along subparallel …

The evolution of volcanic islands is generally marked by fast construction phases alternating
with destruction by a variety of mass-wasting processes. More specifically, volcanic islands …

Dendroclimatic records in areas with high relative humidity and low thermal amplitude are
manifestly scarcer and only a few studies are applied to species that are present in areas …