The partitioning behavior of trace elements is of key importance for understanding the
geochemical process and material cycle mechanism in subduction zones. This paper …

To understand the stability of hydrous phases in mafic oceanic crust under deep subduction
conditions, high-pressure and high-temperature experiments were conducted on two …

The Earth's fluid budget is dominated by species in the system C–O–H–N–S together with
halogens such as F and Cl. H2O is by far the most abundant. Such fluids are one of the two …

Electrical conductivities of the clinopyroxene (Cpx)‐NaCl‐H2O system with various salinities
(5, 10, 15, 20, 25 wt%) and fluid fractions (5, 10, 15, 20, 25 vol%) were measured at 1 GPa …

Aqueous fluids are one of the principal agents of chemical transport in Earth´ s interior. The
precise determination of fluid fractions is essential to understand bulk physical properties …

The dihedral angle (θ) between olivine and aqueous fluid is a critical parameter in
identifying the grain-scale fluid connectivity which controls the distribution and migration of …

摘要微量元素分配对于理解俯冲带地球化学过程及物质循环机制具有重要的意义,
文章总结并重点剖析了以下四个方面的俯冲带微量元素分配问题.(1) 俯冲板片脱水产生的流体 …

Crystallization and solidification pathways in crustal magma chambers control the chemical
and textural evolution of igneous rocks. However, deciphering these codes from completely …

The solubility of Au in silicate melts and fluids governs the enrichment and migration of Au
during the formation of magmatic-hydrothermal Au deposits. Large Au deposits require vast …

The microstructure of realistic fluid–rock systems evolves to minimize the overall interfacial
energy, enabling local variations in fluid geometry beyond ideal models. Consequently, the …