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首页> 外文期刊>Estonian Journal of Earth Sciences >?′13C chemostratigraphy in the upper Tremadocian through lower Katian (Ordovician) carbonate succession of the Siljan district, central Sweden
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?′13C chemostratigraphy in the upper Tremadocian through lower Katian (Ordovician) carbonate succession of the Siljan district, central Sweden

机译:瑞典中部西里扬地区上特马多期至下卡田(奥陶纪)碳酸盐岩的13C化学地层学

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>>Based on ?′13C data from two drillcores recovered from the Siljan district, we present a first continuous carbon isotope record of the upper Tremadocian-lower Katian limestone succession of central Sweden. New names for some isotopic carbon excursions from the Cambrian-Ordovician boundary through the basal Darriwilian are introduced. The Mora 001 core from the western part of the Siljan impact structure ranges through the Lower-Middle Ordovician, whereas the Solberga 1 core from its eastern part ranges through the Middle-lower Upper Ordovician. Upper Tremadocian and Floian units are extremely condensed and include extensive stratigraphic gaps. Multiple hardgrounds, sometimes with minor karstic overprint, imply recurrent periods of erosion and/or non-deposition. Like in other parts of Sweden, the Dapingian and Darriwilian succession is characterized by a relatively complete sedimentary record and low sedimentation rates.
机译:> >基于从西里扬地区回收的两个钻芯的?' 13 C数据,我们提出了瑞典中部特里克多克山-下凯迪安-石灰岩演替的第一个连续碳同位素记录。引入了从寒武纪-奥陶纪边界穿过基底Darriwilian的一些同位素碳偏移的新名称。 Siljan撞击结构西部的Mora 001岩心穿过下奥陶纪中部,而东部Solberga 1岩心则穿过中奥陶纪中下部。上特马多克和弗洛伊安单元高度凝结,并包括大量的地层间隙。多个硬地层,有时有少量的岩溶叠印,意味着反复出现侵蚀和/或不沉积的时期。像瑞典其他地区一样,大坪阶和达里维尔阶演替的特征是相对完整的沉积记录和较低的沉积速率。

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