Iron isotopic fractionation by magmatic-hydrothermal fluid-melt interaction in the Himalayan leucogranites
Year: 2024
Type: article
Abstract: of -0.35‰ successfully explains the observed Fe isotope data. It is likely that these magmatic-hydrothermal fluids are derived from exsolution from the underlying magma reservoirs in the middle crust, which can modify the Fe isotope compositions and bring abundant rare metal elements into the leucogranites. Therefore, Fe isotope data can reveal the properties of magmatic-hydrothermal fluids and serve as an indicator for ore-forming processes.
Source: Fundamental Research
Authors: Yikang Quan, Xia Hu, Dingsheng Jiang, Zhaoqi Ren, Jiaru Sheng, Xiangyu Yan, Yan Jing, Zhikai Xu, Fang Huang
Language: English
Subfield: Geophysics
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: diamond
Award: G7219138246
OpenAlex ID: W4404803086