首页> 外文期刊>Estonian Journal of Earth Sciences >Timing of ductile shearing within the Dr??k??iai-Polotsk Deformation Zone, Lithuania: a U-Pb titanite age
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Timing of ductile shearing within the Dr??k??iai-Polotsk Deformation Zone, Lithuania: a U-Pb titanite age

机译:立陶宛Dr ?? k ?? iai-Polotsk变形区内的韧性剪切时间:U-Pb钛矿年龄

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>A U-Pb dating of titanite from an augen granitoid mylonite in the Dr??k??iai-Polotsk Deformation Zone has yielded a concordant age of 1534 >?± >9 Ma. This light brown titanite follows the foliation in the host rock and was obviously formed during retrogression from amphibolite to epidote-amphibolite facies and coeval mylonitization. Shear zones of the same age are known in southern and central Sweden and in NE Poland. These E-W trending deformation zones accommodate both mafic and granitoid intrusions and are probably related to an extensional period in the Mesoproterozoic evolution in the western part of the East European Craton prior to the 1.50-1.45 Ga Danopolonian orogeny.
机译:> Dr ?? k ?? iai-Polotsk变形区的奥氏花岗岩类钛矿的钛矿的U-Pb测年年龄为1534 >?± > 9马这种浅棕色钛矿跟随叶脉在宿主岩中形成,并且明显是在从闪石到倒影-闪石-岩相的倒退和同代的髓鞘化过程中形成的。在瑞典南部和中部以及波兰东北部,已知相同年龄的剪切带。这些E-W趋势变形带可容纳镁铁质岩体和花岗岩岩体侵入,可能与东欧克拉通西部中元古代生代演化的延伸期早于1.50-1.45伽达波隆造山运动有关。

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