Detrital zircon U-Pb geochronology of the Paleogene Zhu 1 Depression, Pearl River Mouth Basin, China
- Wang, Wei
- Ye, Jiaren
- Bidgoli, Tandis
- Yang, Xianghua
- Shi, Hesheng
- Shu, Yu
Here we report 409 new concordant U-Pb ages from detrital zircons separated from the Paleogene Wenchang, Enping, and Zhuhai formations in the Zhu 1 depression, Pearl River Mouth Basin，South China Sea. The new data, combined with the published age data from the region, document changes in the provenance of syn-rift successions.
How to cite this dataset:
Wang, W., Ye, J., Bidgoli, T., Yang, X., Shi, H., Shu, Y. 2017. Detrital zircon U-Pb geochronology of the Paleogene Zhu 1 Depression, Pearl River Mouth Basin, China, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/100721.
DOI Creation Date:
Wang, W., Ye, J., Bidgoli, T., Yang, X., Shi, H. and Shu, Y., 2017. Using detrital zircon geochronology to constrain Paleogene provenance and its relationship to rifting in the Zhu 1 Depression, Pearl River Mouth Basin, South China Sea. Geochemistry, Geophysics, Geosystems, 18(11), pp.3976-3999.
Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC BY-NC-SA 3.0]
- Coverage Scope: Regional (Continents, Oceans)
- Geographic Location: Pearl River Mouth Basin
User Contributed Keyword(s):
U-Pb, Source-to-sink, South China Block, Wenchang Formation, Yanshanian, geochronology
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