首页> 外文期刊>Journal of Asian earth sciences >Late Cretaceous age of eclogite facies metamorphism of the Sanbagawa belt in the Asemi River area, Shikoku (SW Japan): Evidence from detrital zircon
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Late Cretaceous age of eclogite facies metamorphism of the Sanbagawa belt in the Asemi River area, Shikoku (SW Japan): Evidence from detrital zircon

机译:晚期白垩纪时代eClogite在亚马逊河区的Sanbagawa腰带的变质,Shikoku(SW日本):来自Detrital Zircon的证据

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摘要

Within the Sanbagawa metamorphic belt, the timing of high-pressure and retrograde metamorphism is controversial. Recently, an area in the Asemi River region (central Shikoku, Japan) was delineated that had been subjected to ecologite fades metamorphism prior to retrograde metamorphism in the epidote-amphibolite facies which provides a new opportunity to constrain the age of high-pressure metamorphism. Detrital zircon from this area yields ages as young as 84 +/- 4 Ma. Hence, the protoliths were deposited not earlier than ca. 88 Ma and thus, eclogite facies and retrograde metamorphism occurred after 88 Ma, probably at 86-82 Ma as indicated by the age of metamorphic zircon and K-Ar and Ar-Ar ages for white mica.
机译:在Sanbagawa变形带内,高压和逆行变质的时序是有争议的。近日,在逆行交流面的逆行变质之前,亚洲河流区域(日本中央Shikoku,日本中央Shikoku,日本)的区域被划定了逐渐消退的变质,这为限制高压变质年龄的新机会提供了新的机会。来自该地区的诽谤锆石收益率为84 +/- 4 mA的年龄。因此,促阳糖被沉积而不是比CA更早沉积。 88 mA,因此,88 mA后,eClogite相和逆行变质发生,大概在86-82 mA,如Metalmphic Zircon和K-Ar和白色云母的Ar-Ar Ag。

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