Determining the age of apatite crystals from uranium fission tracks

1991 ◽  
Vol 71 (5) ◽  
pp. 943-945
Author(s):  
Kh. Murtazaev ◽  
V. P. Perelygin ◽  
R. I. Petrova ◽  
S. G. Stetsenko
1967 ◽  
Vol 23 (3) ◽  
pp. 553-555 ◽  
Author(s):  
A. R. Patel ◽  
M. K. Agarwal ◽  
C. C. Desai

Geochronology ◽  
2021 ◽  
Vol 3 (2) ◽  
pp. 561-575
Author(s):  
Peter Klint Jensen ◽  
Kirsten Hansen

Abstract. To enable the separation of pre- and postdepositional components of the length distribution of (partially annealed) horizontal confined fission tracks, the length distribution is corrected by deconvolution. Probabilistic least-squares inversion corrects natural track length histograms for observational biases, considering the variance in data, modelization, and prior information. The corrected histogram is validated by its variance–covariance matrix. It is considered that horizontal track data can exist with or without measurements of angles to the c axis. In the latter case, 3D histograms are introduced as an alternative to histograms of c-axis-projected track lengths. Thermal history modelling of samples is not necessary for the calculation of track age distributions of corrected tracks. In an example, the age equations are applied to apatites with predepositional (inherited) tracks in order to extract the postdepositional track length histogram. Fission tracks generated before deposition in detrital apatite crystals are mixed with post-depositional tracks. This complicates the calculation of the post-sedimentary thermal history, as the grains have experienced different thermal histories prior to deposition. Thereafter, the grains share a common thermal history. Thus, the extracted post-depositional histogram without inherited tracks may be used for thermal history calculation.


2021 ◽  
Author(s):  
Peter Klint Jensen ◽  
Kirsten Hansen

Abstract. Equations for the distribution of age versus length of partially annealed horizontal fission tracks in apatite is presented. Probabilistic least–squares inversion corrects natural track length histograms for observational biases considering the variance of data, modelization, and prior information. The corrected histogram is validated by its variance–covariance matrix. It is considered that horizontal track data can be with or without measurements of angles to the c–axis. In the last case, 3D–histograms are introduced as an alternative to histograms of c–axis projected track lengths. Thermal history modeling of samples is not necessary for track age distribution calculation. In an example the age equations are applied to apatites with pre–depositional (inherited) tracks, to extract the post–depositional track length histogram. Fission tracks generated before deposition in detrital apatite crystals are mixed with post–depositional tracks. This complicates the calculation of the post– sedimentary thermal history as the grains have experienced different thermal histories until deposition. Thereafter the grains share a common thermal history. The extracted post–depositional histogram without inherited tracks may be used for thermal history calculation.


2020 ◽  
Vol 227 ◽  
pp. 02012
Author(s):  
R. S. Sidhu ◽  
R. J. Chen ◽  
Yu. A Litvinov ◽  
Y. H. Zhang ◽  

The re-analysis of experimental data on mass measurements of ura- nium fission products obtained at the ESR in 2002 is discussed. State-of-the-art data analysis procedures developed for such measurements are employed.


1963 ◽  
Vol 101 (2) ◽  
pp. 215-224 ◽  
Author(s):  
W.F. Neuman ◽  
R. Bjornerstedt ◽  
B.J. Mulryan

1984 ◽  
Vol 2 (2) ◽  
pp. 227-252 ◽  
Author(s):  
F. Macášek ◽  
P. Rajec ◽  
R. Kopunec ◽  
V. Mikulaj

2006 ◽  
Vol 41 (3) ◽  
pp. 268-275 ◽  
Author(s):  
S. N. Danilchenko ◽  
A. V. Koropov ◽  
I. Yu. Protsenko ◽  
B. Sulkio-Cleff ◽  
L. F. Sukhodub

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