ABSTRACT The widespread Cenozoic Himalayan leucogranites (HLs) are representative
rocks evolving from relatively pure crust-derived melts with few mantle material inputs and …

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 …

The generation, transport, and recrystallization of slab-derived melts/fluids play a critical role
in the deep recycling of elements in subduction zones. While boron (B) isotope systematics …

Two-mica granite is the most common magmatic rock type in the Himalayan leucogranite
belt, which has close relationship with rare metal mineralization. Its genesis is generally …

Crustal rocks in collisional orogens often underwent the metamorphic transition from
dehydration to anatexis in response to an increase of geothermal gradients, but it remains …

Boron (B) isotopes are widely used in studies of water–rock interaction and earth surface
processes. The δ 11 B is a potentially attractive proxy of seawater pH, as the relative …

The geochemistry of granite is largely controlled by physical and chemical parameters that
are closely linked to tectonic processes in evolving orogenic belts. Therefore, temporal …

Multi-component crustal sources are universally acknowledged as the overriding factor in
causing geochemical heterogeneities of the Cenozoic Himalayan leucogranites. In previous …

The origins of Cenozoic granites in the Himalaya are key to understanding the evolution of
the Himalayan orogen. However, it is unclear whether these granites represent primary …

Boron geochemistry can track fluid–rock interaction during metamorphic evolution and
provides important insights into mass transfer processes in subduction zones. This study …