首页> 外文期刊>Bulletin of geosciences >The Geniai Tuff in the southern East Baltic area - a new correlation tool near the Aeronian/Telychian stage boundary, Llandovery, Silurian
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The Geniai Tuff in the southern East Baltic area - a new correlation tool near the Aeronian/Telychian stage boundary, Llandovery, Silurian

机译:东波罗的海南部地区的Geniai Tuff –一种新的相关工具,位于志留纪Alanderian / Telychian阶段边界,Llandovery附近

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In three drill cores in Latvia and Lithuania a thin (1 cm thick) altered volcanic ash bed with high concentrations of phosphorus (up to 3%), cerium (1%), lanthanum (0.5%) and strontium (2.5%), has been found close to the Aeronian/Telychian boundary (Llandovery, Silurian, ca 438 Ma). Small, millimetre-thick lenses within the ash bed contain up to 12% P and Sr, up to 6% Ce and 3% La. These elements occur as a solid solution of goyazite-florencite mineral. Additionally, authigenic K-feldspar and kaolinite occur in this ash bed. The high concentrations of REE elements, strontium and phosphorus suggest a carbonatite source magma, but the strontium isotope ratio contradicts that origin. Such a unique composition in a volcanic ash layer is a good basis for using it as a marker horizon for correlation of sections.
机译:在拉脱维亚和立陶宛的三个钻探岩心中,一个薄的(1厘米厚)蚀变的火山灰床含高浓度的磷(高达3%),铈(1%),镧(0.5%)和锶(2.5%)。被发现靠近Aeronian / Telychian边界(Llandovery,志留纪,约438 Ma)。烟灰床上的毫米毫米厚的小透镜含有高达12%的P和Sr,高达6%的Ce和3%的La。这些元素以方沸石-堇青石矿物的固溶体形式存在。此外,自生钾长石和高岭石也出现在该灰床中。稀土元素,锶和磷的高浓度表明是碳酸盐岩源岩浆,但锶同位素比与该成因相矛盾。火山灰层中如此独特的成分是将其用作剖面关联的标记层的良好基础。

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