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首页> 外文期刊>Resource Geology >SHRIMP U-Pb Zircon Age of the Inishi Migmatite around the Kamioka Mining Area, Hida Metamorphic Complex, Central Japan
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SHRIMP U-Pb Zircon Age of the Inishi Migmatite around the Kamioka Mining Area, Hida Metamorphic Complex, Central Japan

机译:日本中部飞ida变质综合体神冈矿区附近的Inishi芒硝的SHRIMP U-Pb锆石年龄

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摘要

SHRIMP U-Pb ages were determined on single zircons separated from the Inishi migmatite in the Kamioka mining area, Hida metamorphic complex, central Japan. Twenty one determinations were distributed within the age of 234.2±1.8 Ma, excluding one inner core of a grain. As the analyzed crystals were mostly euhedral igneous zircons, the age indicates the crystallization of zircons from granitic melt during the formation of Inishi migmatite. The age of ca. 234 Ma corresponded to the later stage of the major regional metamorphic event in the Hida complex, while the age of ca. 265 Ma determined in a grain suggested the inherited age of the earlier phase of the metamorphism.
机译:在日本中部飞ida变质综合体Kamioka矿区,从Inishi migmatite分离出的单个锆石确定了SHRIMP U-Pb年龄。 21个测定值分布在234.2±1.8 Ma的年龄范围内,不包括谷物的一个内核。由于分析的晶体大多为真面状火成锆石,因此年龄表明在Inishi辉锰矿形成过程中,锆石从花岗岩熔体中结晶出来。大约年龄。 234 Ma对应于飞ida(Hida)复合体中主要区域变质事件的后期,而其年龄大约为。确定的265 Ma暗示了变质作用早期阶段的遗传年龄。

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