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首页> 外文期刊>Geological Quarterly >Badenian tuffite levels within the Carpathian orogenic front (Gdow–Bochnia area, Southern Poland): radio-isotopic dating and stratigraphic position
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Badenian tuffite levels within the Carpathian orogenic front (Gdow–Bochnia area, Southern Poland): radio-isotopic dating and stratigraphic position

机译:喀尔巴阡山造山带前锋(格多-波奇尼亚地区,波兰南部)内的巴登尼亚凝灰岩含量:放射性同位素测年和地层位置

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摘要

We present new results of investigation of Middle Miocene Badenian tuffite levels exposed in Southern Poland within the Gdow " embayment" area (tuffites from Wiatowice, upper part of the Skawina Beds, foraminiferal biozone Ⅱγ) and compare them with the well known and extensively described Bochnia Tuffite level at Chodenice near Bochnia (upper part of the Chodenice Beds, foraminiferal biozone ⅢA). The ~(40)Ar/~(39)Ar ages of the glass separates obtained from these layers were determined applying (standard) incremental heating techniques the Wiatowice and Bochnia tuffites have been dated to be 13.76 ±0.08 Ma, and 13.62 ±0.10 Ma old, respectively.
机译:我们提出了在波兰南部格多(Gdow)“隔离区”内暴露的中新世中新世巴德尼亚凝灰岩含量的新结果(凝灰岩来自Wiatowice,Skawina层上部,有孔虫生物区Ⅱγ),并将其与广为人知的Bochnia进行了比较Bochnia附近的Chodenice的凝灰岩水平(Chodenice床的上部,有孔虫生物区ⅢA)。从这些层获得的玻璃隔板的〜(40)Ar /〜(39)Ar年龄是使用(标准)增量加热技术确定的,Wiatowice和Bochnia凝灰岩的日期已定为13.76±0.08 Ma,和13.62±0.10 Ma旧的。

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