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首页> 外文期刊>Doklady Earth Sciences >The Lower-Middle Riphean Boundary in the Southern Urals: New Isotopic U-Pb (SHRIMP II) Constraints
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The Lower-Middle Riphean Boundary in the Southern Urals: New Isotopic U-Pb (SHRIMP II) Constraints

机译:乌拉尔南部的中下部里菲安边界:新的同位素U-Pb(SHRIMP II)约束

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摘要

In the general Precambrian stratigraphic scale of the former USSR approved at the 2nd All-Russia meeting on general problems of Precambrian stratigraphy (Ufa, 1990), the Riphean representing the largest Upper Pro-terozoic subdivision comprises three chronostrati-graphic units—the Lower Riphean (Burzyanian), Middle Riphean (Yurmatinian), and Upper Riphean (Kara-tavian)—with the lower isotopic boundaries at 1650 ± 50, 1350 ± 20, and 1000 ± 50 Ma, respectively . The Riphean-Vendian boundary is placed at 650 ± 20 Ma.
机译:在前苏联在第二次全俄关于前寒武纪地层一般问题会议上批准的前寒武纪地层总规模中(Ufa,1990),代表最大的上元古界细分的里菲安包括三个年代地层单位-下里菲安(布尔兹亚尼),中里菲亚(Yurmatinian)和上里菲亚(Kara-tavian)的同位素下界分别为1650±50、1350±20和1000±50 Ma。 Riphean-Vendian边界位于650±20 Ma。

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