Zircon U-Pb and reassessed zircon fission track ages of Miocene Mizunami and Iwamura Groups in the southeastern part of Gifu Prefecture, central Japan

E. Sasao, T. Danhara, H. Iwano, T. Hirata
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引用次数: 1

Abstract

Here U–Pb and reassessed fission track (FT) ages are presented for samples from the Miocene Mizunami and Iwamura groups in the southeastern Gifu Prefecture, central Japan. The U–Pb ages of three tuff samples coincide with the reassessed FT ages within the error range. These new U–Pb and reassessed FT ages are consistent with those reported in previous microfossil and paleomagnetic studies, which indicate the following depositional history: The Hongo and Akeyo formations of the Mizunami Group were deposited at ~19–18 Ma and ca. 18 Ma, respectively, and the lower part of the Toyama Formation of the Iwamura Group was deposited ca. 18 Ma.
日本中部岐阜县东南部中新世Mizunami和Iwamura群锆石U-Pb和锆石裂变径迹年龄的重新评估
本文介绍了日本中部岐阜县东南部中新世Mizunami和Iwamura组样品的U-Pb和重新评估的裂变径迹(FT)年龄。3个凝灰岩样品的U-Pb年龄与重新评估的FT年龄在误差范围内一致。这些新的U-Pb和重新评估的FT年龄与前人的微化石和古地磁研究结果一致,表明了以下沉积历史:水南群Hongo组和Akeyo组沉积时间分别为~ 19-18 Ma和约18 Ma,岩村群富山组下部沉积时间约为18 Ma。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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