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首页> 外文期刊>Tectonics >The ~(40)Ar/~(39)Ar dating of magmatic activity in the Donbas Fold Belt and the Scythian Platform (Eastern European Craton)
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The ~(40)Ar/~(39)Ar dating of magmatic activity in the Donbas Fold Belt and the Scythian Platform (Eastern European Craton)

机译:Donbas褶皱带和Scythian平台(东欧克拉通)中岩浆活动的〜(40)Ar /〜(39)Ar测年

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摘要

The Donbas Fold Belt is the compressionally deformed southeasternmost part of the intracratonic late Paleozoic Dniepr-Donets rift basin. It is situated in an intracratonic setting but close to the southern margin of the East European Craton, south of which lies the Scythian Platform. A range of igneous rocks from the Donbas Fold Belt and the Scythian Platform were dated by the ~(40)Ar/~(39)Ar method in order to constrain the ages of magmatic activity in these areas, and compare them. The plateau ages from the south margin of the Donbas Fold Belt vary from 151.4 +-4.7 Ma to 278.1 +- 5.3 Ma, and define three main age groups: Middle-Late Jurassic, Middle-Late Triassic, and Early Permian.
机译:顿巴斯褶皱带是克拉通晚期古生代第聂伯-顿涅茨裂谷盆地的最南端压缩变形的部分。它坐落在克拉通内,但靠近东欧克拉通的南缘,其南部是Scythian平台。为了限制这些地区的岩浆活动年龄,并通过〜(40)Ar /〜(39)Ar方法对Donbas褶皱带和Scythian平台上的一系列火成岩进行了测年。 Donbas褶皱带南缘的高原年龄从151.4 + -4.7 Ma到278.1 +-5.3 Ma不等,并定义了三个主要年龄组:侏罗纪中晚期,三叠纪中晚期和二叠纪早期。

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