Fission-track dating using both internal and external surfaces of zircons was carried out for ten core samples from the Miocene formations in the Ayukawa-Yurihara district, Akita Prefecture. These samples were collected from the Yashiozawakawa, Nishikurosawa and Onnagawa Formations of eight wells drilled for the petroleum exploration in this area.
After the detail examination for grain ages of each sample using histogram, age spectrum and radial plot, fission-track ages are interpretated. The results are summarized as follows.
1) Although external fission-track age (20.1 ± 1.3Ma) of andesite in the upper part of the Yashiozawakawa Formation shows the eruption age with some possibility of rejuvenation, internal fission-track age (16.4 ± 0.6Ma) shows the thermal event which probably corresponds to the start of the “graben-fill basalt” activity.
2) The most reliable internal fission-track age (12.2 ± 0.4Ma) of acidic tuff in the Nishikurosawa Formation is in harmony with the biostratigraphic age of this formation. The external fission-track age (16.6 ± 0.8Ma) indicates that the provenance of zircons is probably the Hatamura Formation.
3) The most reliable fission-track age of tuffs between the O-1 and O-2 benthonic foraminiferal assemblages, 8.6 ± 0.4 Ma of the Ayukawa-kita well, is consistent with Sr isotopic age (about 9Ma) of the O-2 assemblage. The age of the O-1 assemblage is estimated 8.2 Ma based on K-Ar ages of the overlying Fukuyama andesite. Therefore, the O-1 assemblage is correlated with “Blue zone” in Niigata Prefecture, and has a possibility of regional correlation marker.
4) This study indicates that the fission-track dating using both surfaces and more than one samples of the same horizon is a valuable method for the use of few and expensive cores.
View full abstract