Porphyry deposits are large, low-grade metal ore bodies that are formed from hydrothermal
fluids derived from an underlying magma reservoir. They are important as major sources of …

Metals such as Cu, Mo, Au, Sn, and W in porphyry and related epithermal mineral deposits
are derived predominantly from the associated magmas, via magmatic–hydrothermal fluids …

The hydration and complexation of metals in hydrothermal fluids are key processes
controlling the mobility of elements in the Earth's crust, leading to the formation of ore …

Most of the global Sn resources are from granite-related ore deposits, which form in
response to cassiterite precipitation from hydrothermal fluids. However, the physical and …

Economically exploitable deposits of metallic minerals (ore deposits) form in the Earth's crust
through a variety of geologic processes. These involve extraction of metals at low …

This contribution provides an overview of available experimental, thermodynamic, and
molecular data on Au aqueous speciation, solubility, and partitioning in major types of …

Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) has become a
most powerful technique for the elemental analysis of individual, polyphase inclusions …

Geological aqueous fluids operate in a wide range of temperatures (from 0 to 1000 C) and
depths (from Earth surface to~ 10s km), over which the physical-chemical properties of water …

Current models of the formation and distribution of gold deposits on Earth are based on the
long-standing paradigm that hydrogen sulfide and chloride are the ligands responsible for …

The Tethyan metallogenic domain (TMD), as one of the three major domains in the world,
extends over 10000 km from east to west, and has developed several world-class …