Whole-rock elemental and Sr-Nd-Hf-Pb-Fe isotopic evidence for the Initial ‘return’ of recycled paleo-Pacific oceanic crust observed in the early Cretaceous (~123 Ma) intraplate magmatism from eastern China

Creator(s):
Jiang, Dingsheng
Xu, Xi-sheng
Wang, Xiao-Jun
Huang, Fang
Zeng, Gang
Chen, An-Xia
Huang, Bei
Abstract:
With the aim to seek if subducted paleo-Pacific slab had ‘returned’ through Mesozoic magmatism, we focus on an early Cretaceous (~123 Ma) diabase with OIB affinities in eastern China and provide robust whole-rock elemental and Sr-Nd-Hf-Pb-Fe isotopic evidence.
How to cite this dataset:
Jiang, D., Xu, X., Wang, X., Huang, F., Zeng, G., Chen, A., Huang, B., 2022. Whole-rock elemental and Sr-Nd-Hf-Pb-Fe isotopic evidence for the Initial ‘return’ of recycled paleo-Pacific oceanic crust observed in the early Cretaceous (~123 Ma) intraplate magmatism from eastern China, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111721. Accessed 2021-09-20.
DOI Creation Date:
2020-10-27
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC BY-SA 4.0]
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Eastern China
User Contributed Keyword(s):
recycled oceanic crust; terrigenous sediments; Fe stable isotope; paleo-Pacific plate subduction; eastern China
Data Available On:
2022-01-01
Resource Type:
Collection
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