Timing of mylonitization in the Nihonkoku Mylonite Zone of north Central Japan: Implications for Cretaceous to Paleogene sinistral ductile deformation in the Japanese Islands

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• 作者：Yutaka Takahashi^a ; ^{takahashi-yutaka@aist.go.jp} ; Jianren Mao^b ; Xilin Zhao^b
• 关键词：Nihonkoku Mylonite Zone ; SHRIMP U&ndash ; Pb age ; K&ndash ; Ar age ; Zircon ; Biotite ; Hornblende
• 刊名：Journal of Asian Earth Sciences
• 出版年：2012
• 期刊代码：40_13679120
• 类别：ear
• 出版时间：30 March, 2012
• 卷：47
• 期：Complete
• 页码：265-280
• 文件大小：5559 K

摘要

The Nihonkoku Mylonite Zone is one of the Cretaceous to Paleogene sinistral ductile shear zones in the Japanese Islands, which branches off from the Tanagura Tectonic Line (TTL). The Nihonkoku Mylonites are composed mainly of hornblende-biotite granodiorite mylonite, biotite granodiorite mylonite, and biotite granite mylonite, derived from Late Cretaceous to Paleogene granitic rocks in the Ashio Belt. SHRIMP U-Pb analyses of zircon from the Nihonkoku Mylonites yield ages of 63-67 Ma. K-Ar ages obtained for biotite of the Nihonkoku Mylonites are 46-52 Ma. The SHRIMP U-Pb ages of zircon indicate the ages of consolidation of the granitic magmas, whereas the K-Ar ages indicate the ages of cooling of granitic plutons. Mylonitization occurred under conditions of the upper greenschist to amphibolite facies, deduced from recrystallization of biotite and generation of myrmekite around porphyroclasts of alkali feldspar. Based on these results, the magmas of the parent rocks of the Nihonkoku Mylonites were intruded and consolidated at around 65 Ma, and mylonitization occurred at around 55-60 Ma, timing of which is correlative to the low-temperature deformation that occurred after 60-70 Ma along the TTL, subsequent to the main mylonitization.