As prototypes of crust-derived remelted S-type granite, Himalayan leucogranites have
considerable relevance in crustal evolution and associated metallogeny. However, given …

Interpreting isotopic signatures documented in natural rocks requires knowledge of
equilibrium isotopic fractionation factors. Here, we determine equilibrium Fe isotope …

Magnesium isotopic fractionation during basalt differentiation is commonly thought to be
negligible at current levels of analytical precision. However, Mg isotopic variation of∼ …

Crystal-melt separation is important for understanding the evolution of granitic magma and
the connection between plutonic and volcanic rocks. Crystal accumulation and melt …

Partial melts derived from crustal anatexis exhibit large variations in field characteristics,
composition, and isotope geochemistry. The relative influence of melting process and …

喜马拉雅淡色花岗岩世界瞩目, 具有重要的理论研究和找矿意义, 但是其成因争议较大.
本文统计了两千余件样品的全岩主微量地球化学, Sr-Nd-Pb-Hf 同位素, 锆石/独居石/磷钇矿等副 …

Rationale Zinc isotopes are becoming increasingly applicable in high‐temperature
geochemistry, for example in crust–mantle interaction and volatilization‐related processes …

As an important post-collisional magmatic product in the orogenic belt, the Himalayan
leucogranites are the critical host rocks for a number of rare-metal mineralization (such as Li …

The geological evolution of orogens is the sum of events related to both their cycle of
generation as well as features inherited from their basement units. The Himalayan Orogen …

Zinc (Zn) is an essential micronutrient, and its isotopes are increasingly applied to
understand trace metal biogeochemical cycling. Atmospheric deposition from anthropogenic …