The age of sample can be obtained by using this equation, age = N × Ds/Di × 6 × 10−8, in which N is the total neutron dose expressed as neutrons per square centimetre and Ds is the observed track density for spontaneous fission while Di is that for induced fission.
Fission Track Dating Constants: λ"-1.55 125 x 10"。у'. Af = 8.46 × 10.17 yı:o-580.2 x 10'24 cm2. 235Upsv- 1/137.88 3. Muscovite from Val Grosina in the Swiss Alps was dated by...
Fission Track Dating Constants: λ"-1.55 125 x 10"。у'. Af = 8.46 × 10.17 yı:o-580.2 x 10'24 cm2. 235Upsv- 1/137.88 2. Church and Bickford (1971, Geol. Soc. Amer. Bul., 82:1727-1734) analyzed an apatite in the granite of the Sawatch Range of Colorado. The granite has a whole-rock Rb-Sr date of 1650 x 10 years. The rock sample from which the apatite was taken yielded a Rb-Sr mineral- isochron date of 1275x 106 years. The analytical results for the apatite (A38G-II, 4)...
Fission Track Dating Constants: λ"-1.55 125 x 10"。у'. Af = 8.46 × 10.17 yı:o-580.2 x 10'24 cm2. 235Upsv- 1/137.88 2. Church and Bickford (1971, Geol. Soc. Amer. Bul., 82:1727-1734) analyzed an apatite in the granite of the Sawatch Range of Colorado. The granite has a whole-rock Rb-Sr date of 1650 x 10 years. The rock sample from which the apatite was taken yielded a Rb-Sr mineral- isochron date of 1275x 106 years. The analytical results for the apatite (A38G-II, 4)...