Geochemistry data of the Early Cretaceous Siling gabbro and Daixi granite from the Gan-Hang Belt (South China)
In seeking to clarify the crust-mantle architecture within cratonic foreland associated with arc accretion, we carried out a systematic study on whole-rock geochemistry, zircon U-Th-Pb, and zircon Hf-O isotopes of the Eary Cretaceous Siling gabbro and Daixi granite from the Ganhang Belt (South China).
How to cite this dataset:
Jiang, D., 2020. Geochemistry data of the Early Cretaceous Siling gabbro and Daixi granite from the Gan-Hang Belt (South China), Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/111358.
DOI Creation Date:
Jiang, D.S., Xu, X.S., Li, X.L. and Xia, Y., 2020. Emplacement of young island arc crust over older mantle along a cratonic foreland: constraints from multiple isotopes and elemental geochemistry. Journal of Geophysical Research: Solid Earth, 125(8), p.e2019JB018550.
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
National Science Foundation: 9314400
National Science Foundation: 0074868
National Science Foundation: 0001826
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Gan-Hang Belt, South China
User Contributed Keyword(s):
isotope inversion; young arc crust; ancient SCLM; arc obduction
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