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 Yu

Description

Ca-Zn isotope of alkaline rocks

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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

Funders

  • Key R&D Program of China
    Grant ID: 2019YFA0708400
  • MOST special funds of the State Key Laboratory of Geological Processes and Mineral Resources
    Grant ID: MSFGPMR01

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