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Furthermore, the Cenozoic fission track ages and modeling fission track data suggest that pre-breakup basins may have covered the outer coast.
Zircon fission track (ZFT), apatite fission track (AFT) and (U Th)/He thermochronometric data are used to reconstruct the Cenozoic exhumation history of the South China continental margin.
Fission track thermochronometry data are often a core element of modern tectonic and denudation studies.
Fission track dating has greatly expanded its usefulness to geology over the last 40 years.
We found for all samples that the fully automated fission track counting procedure using the Autoscan System yields a larger scatter in the measured fission-track densities compared to conventional (manual) track counting.
Combining fission track analysis with cosmogenic nuclide decay rates, one can study landscape development and denudation of passive margins.
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Compare fission-track dating.
Brandon, M.T., 1992, Decomposition of fission-track grain-age distributions.
W.E., 1983, Confidence limits for fission-track dating.
This approach is essential for estimating ages for young fission-track samples.
Used to calculates zeta or Z factor for fission-track data using an age standard.
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