Thermal Annealing Characteristics of Detrital Zircon Fission Track Obtained from Natural Borehole Samples
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-021-1512-1.pdf
Reference40 articles.
1. Bernet, M., Garver, J. I., 2005. Fission-Track Analysis of Detrital Zircon. Reviews in Mineralogy and Geochemistry, 58(1): 205–237. https://doi.org/10.2138/rmg.2005.58.8
2. Bernet, M., 2009. A Field-Based Estimate of the Zircon Fission-Track Closure Temperature. Chemical Geology, 259(3/4): 181–189. https://doi.org/10.1016/j.chemgeo.2008.10.043
3. Cai, C. E., Qiu, N. S., Li, H. L., et al., 2020. Study of the Closure Temperature of (U-Th)/He in Detrital Zircon Obtained from Natural Evolution Samples. Science China Earth Sciences, 63(3): 412–424. https://doi.org/10.1007/s11430-019-9450-0
4. Chen, Z. Q., Shi, G. R., 2003. Late Paleozoic Depositional History of the Tarim Basin, Northwest China: An Integration of Biostratigraphic and Lithostratigraphic Constraints. AAPG Bulletin, 87(8): 1323–1354. https://doi.org/10.1306/0401032001115
5. Craddock, W. H., Moore, T. E., O’Sullivan, P. B., et al., 2018. Late Cretaceous-Cenozoic Exhumation of the Western Brooks Range, Alaska, Revealed from Apatite and Zircon Fission Track Data. Tectonics, 37(12): 4714–4751. https://doi.org/10.1029/2018tc005282
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