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Wenlock bentonites in Lithuania and correlation with bentonites from sections in Estonia, Sweden and Norway

机译:立陶宛的温洛克膨润土及其与爱沙尼亚,瑞典和挪威的部分膨润土的相关性

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摘要

Seven Wenlock bentonite beds from four drill cores in Lithuania with sufficient thickness for sampling were analysed by XRD and XRF. The sanidine composition of bentonites combined with graptolite biozonation of the host rock were used for correlations. Two of the studied bentonite samples at the antennularius/flexilis biozone boundary can be confidently correlated between two Lithuanian sections. Four of the studied bentonites can be correlated with lower or higher probability with earlier studied bentonites in Estonia and Sweden. Identification of the Grotlingbo Bentonite in the Vidukle-61 drill core, and descriptions of other east Baltic sections enables composition of it thickness map of the Grotlingbo Bentonite. The thickness pattern with two axes, and the layered composition of the Grotlingbo Bentonite, indicate a change of the wind direction during a long lasting eruption. Hypothetical location of the volcanic source in the Silurian was within the zone of the Baltica-Laurentia collision.
机译:XRD和XRF分析了来自立陶宛四个钻芯的七个Wenlock膨润土床,其厚度足以进行采样。膨润土的Sanidine成分与基质岩石的角砾岩生物区带相结合。可以在两个立陶宛剖面之间可靠地关联到在tentenularius / flexilis生物区边界处的两个膨润土样品。在爱沙尼亚和瑞典,四个被研究的膨润土与早期研究的膨润土的可能性较低或较高相关。通过识别Vidukle-61钻芯中的Grotlingbo膨润土,以及对其他波罗的海东部地区的描述,可以构成Grotlingbo膨润土的厚度图。带有两个轴的厚度模式以及Grotlingbo膨润土的层状组成表明在长期喷发期间风向发生了变化。志留纪中火山源的假想位置位于波罗的海-劳伦蒂亚碰撞带内。

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