Platinum-group elements (PGEs) have a strong affinity for sulfur and tend to accumulate in
the deep continental crust, either concentrated within magmatic Cu-Ni-PGE deposits or …

Mantle oxidation plays an essential role in volatile cycling between Earth's interior and
exterior. However, the conceivable oxidizer remains enigmatic and needs to be explored by …

The geodynamic regime that formed Archean silicic continental crust is unclear. The
episodic Archean TTGs (tonalite–trondhjemite–granodiorite rocks) and associated …

Unlike their eruptive counterparts, plutonic rocks often experience post-cumulus evolution
prior to their final solidification. These processes have the potential to exert significant …

Stable Sn isotope ratios are emerging as a novel tracer for a wide range of geological
processes; however, the Sn isotopic baseline of the upper continental crust (UCC) is not yet …

The Tengchong volcano field (TVF), situated at the southeastern margin of the Tibetan
Plateau, holds crucial information regarding Cenozoic volcanic activities and geotectonic …

Beyond its economic value, copper (Cu) serves as a valuable tracer of deep magmatic
processes due to its close relationship with magmatic sulfide evolution and sensitivity to …

Recent models of solar system formation suggest that a dynamical instability among the
giant planets happened within the first 100 Myr after disk dispersal, perhaps before the …

Copper and iron isotopic signatures in sulfide and silicate minerals are important genetic
indicators in magmatic sulfide deposits. Kalatongke is a large‐scale magmatic Cu‐Ni sulfide …

Explosive eruptions are frequently triggered by mixing of contrast-type magmas such as
mantle-derived basaltic magmas with hydrous silica-rich magmas. Up to date, the …