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 …

Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …

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 …

Magmatic arcs are terrestrial environments where lithospheric cycling and recycling of
metals and volatiles is enhanced. However, the first-order mechanism permitting the …

The metasomatized sub-continental lithospheric mantle (SCLM) is increasingly proposed to
play a key control in the formation of giant gold (Au) deposits. However, the extent of Au …

Much of the world's supply of battery metals and platinum group elements (PGE) comes from
sulphide ore bodies formed in ancient sub-volcanic magma plumbing systems. Research on …

The transfer of chalcophile metals across the continental lithosphere has been traditionally
modeled based on their chemical equilibrium partitioning in sulfide liquids and silicate …

For decades, there has been debate surrounding the transport of dense metal-rich sulfide
liquid in mafic magmas. This topic is crucial to understanding the genesis of valuable …

Abstract Supercritical CO2 (SC CO2), as one of the unique fluids that possess fascinating
properties of gas and liquid, holds great promise in chemical reactions and fabrication of …

With the aim of constraining the influence of the surrounding plates on the Late Paleozoic–
Mesozoic paleogeographic and tectonic evolution of the southern North China Craton …