Magnesium (Mg) has an atomic number of 12 and belongs to the alkaline earth element
(Group II) of the Periodic Table. The pure Mg is a silvery white metal and has a melting point …

Carbon Dioxide removal from air (CDR) combined with permanent solid storage can be
accomplished via carbon mineralization in ultramafic rocks in at least four ways: 1. Surficial …

The dissolution rates of olivine have been considered by a plethora of studies in part due to
its potential to aid in carbon storage and the ease in obtaining pure samples for laboratory …

Dolomite precipitation models and kinetics are debated and complicated due to the complex
and temporally fluctuating fluid chemistry and different diagenetic environments. Using well …

In order to better constrain the Mg isotopic composition of the mantle, we have analysed
twenty-eight samples of both oceanic and continental peridotite using a high-precision …

Serpentinite plays a crucial role in element mobility during seawater hydrothermal alteration
of mid-ocean ridge peridotite on the seafloor and fluid metasomatism of peridotite in the …

Magnesium isotopic compositions of igneous rocks could be potentially used to trace
recycling of supracrustal materials. High-δ 26 Mg granitoids have been previously reported …

We present high-precision Fe and Mg isotopic data for the Purang ophiolite, southwestern
Tibet, representing the first combined Fe and Mg isotopic study of the oceanic lithosphere …

In recent years, the mélange model has been increasingly considered as an important way
to transfer slab components to arc sources in modern subduction zones. This model differs …

The magnesium isotope compositions of sedimentary carbonates are widely used to
investigate the geochemical cycling of this element in seawater. Density Functional Theory …