This review focuses on the solubility, origin, abundance, and degassing of carbon dioxide
(CO 2) in magma–hydrothermal systems, with applications for those workers interested in …

Carbon emission at volcanic centers requires a constant balance between output (mostly by
volcanism, either at plate boundaries or intraplate) and input (mostly at trench settings) of …

The influence of water on the dynamics of the oceanic upper mantle is re-evaluated based
on recent experimental constraints on the solubility of water in mantle minerals and earlier …

This remarkable volume presents the first revision to the classification system of diamond-
bearing rocks in over eighty years. Presenting the latest mineralogical data, this book offers …

The onset of partial melting beneath mid-ocean ridges governs the cycling of highly
incompatible elements from the mantle to the crust, the flux of key volatiles (such as CO2, He …

Major and trace element and Sr–Nd–Pb–O–C isotopic compositions are presented for
carbonatites from the Cape Verde (Brava, Fogo, Sáo Tiago, Maio and Sáo Vicente) and …

Carbonatites are redefined using a mineralogical-genetic classification and divided into two
groups: primary carbonatites, and carbothermal residua. Attention is drawn to the fact that …

We present partial melting experiments that constrain the near solidus phase relations of
carbonated eclogite from 2 to 8.5 GPa. The starting material was prepared by adding 5 wt …

Fluid-inclusions in fibrous diamonds from Jwaneng (Botswana) contain water, carbonates,
silicates, apatite, and CO 2. Average compositions of fluids trapped in individual diamonds …

Bulk-rock geochemical compositions of hypabyssal kimberlites, emplaced through the
Archaean Kaapvaal craton and Proterozoic Namaqua–Natal belt, are used to estimate close …