Mantle compositional-spatial variations caused by oblique subduction of calcium carbonate: Insights from decoupled Ca-Zn isotopes of alkaline rocks
Published: 27 December 2023| Version 1 | DOI: 10.17632/gwgnsjmfbj.1
Contributor:
kaizhang YuDescription
Ca-Zn isotope of alkaline rocks
Files
Steps to reproduce
Major elements were analyzed by X-ray fluorescence at State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (GPMR-CUG) in Wuhan. Trace elements were analyzed using an Agilent 7700x inductively coupled plasma mass spectrometer (ICP-MS) at GPMR-CUG. Ca-Zn isotopic compositions were determined by Triton TIMS and MC-ICP-MS at GPMR-CUG.
Institutions
China University of Geosciences
Categories
Geochemistry
Funding
Key R&D Program of China
2019YFA0708400
National Natural Science Foundation of China
42303049
MOST special funds of the State Key Laboratory of Geological Processes and Mineral Resources
MSFGPMR01