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

The enigmatic geodynamic processes involved in the India-Asia collision shape our
understanding of uplift and deformation of the Tibetan Plateau and the subsequent changes …

Although deep magmatic fluids are important for the shallow magmatic-hydrothermal
evolution and transport/enrichment of ore-forming elements in transcrustal magmatic system …

喜马拉雅新生代淡色花岗岩记录了地壳深熔作用和花岗岩侵位的地球化学和构造物理效应.
与形成于增厚地壳条件下和伸展背景下的始新世和中新世花岗岩相比, 渐新世花岗岩分布比较 …

Serpentinites in subduction zones are important fluid reservoirs for crust-mantle interaction
and arc magma formation. The serpentinite-derived fluids can carry fluid-mobile elements …

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 …

Hydrothermal alteration is crucial in the formation of many ore deposits, with potassium (K)
mobilization and cycling being prevalent. Potassic metasomatism of wall rocks generally …

Vein-type and greisen-type beryllium (Be) mineralization is closely associated with the
magmatic-hydrothermal evolution in highly fractionated granites. However, the source of ore …

Stable barium (Ba) isotopes are emerging as tracers for the recycling of crustal material into
the mantle. Small but significant Ba isotope variations have been found in global MORB (δ …

Most economically important tungsten (W) deposits are of magmatic-hydrothermal origin.
The species and partitioning of W during fluid exsolution, considered to be the controlling …