Amphibole (Amp) plays a crucial role in the study of several earth and planetary processes.
One of its most common applications is in thermobarometry, especially for volcanic …

Phanerozoic orogenic gold mineralization at craton margins is related to the metasomatism
of the lithospheric mantle by crustal material. Slab subduction transfers Au from the crust to …

Thermometry of high-grade metamorphic rocks is difficult due to fast cationic diffusion during
slow cooling, but the titanium content of calcium amphibole (Ti-Amp) can retrieve amphibole …

This article reports a protocol on the application of Amp-TB2 (single-amphibole
thermobarometry) based on detailed electron-microprobe analyses performed on …

We present a new method for calculating amphibole formula from routine electron
microprobe analysis (EMPA) data by applying a principal components regression (PCR) …

Syneruptive magma mixing is widespread in volcanic eruptions, affecting explosivity and
composition of products, but its evidence in basaltic systems is usually cryptic. Here we …

Oxygen fugacity (f O2) is a critical factor that controls the formation mechanisms of the
porphyry Cu deposits. However, the differentiation of the f O2 in post-collisional Au …

The origin of the Eastern Mexican Alkaline Province has been explained by landward arc
migration and subsequent asthenospheric upwelling after slab roll-back of the Farallon …

Magmatic fluid degassing within shallow magma chambers underneath the ore bodies is
critical to the formation of porphyry Cu-Au deposits (PCDs). Yet, it remains unclear how the …

Fractionation of sulfides during ascent of mantle-derived magmas distributes sulfur and
chalcophile elements into the Earth's lithosphere. It has been suggested that continental …