白俄罗斯东南部的上泥盆世岩浆复合体

O. Kuzmenkova, A. Laptsevich, A. Nosova
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引用次数: 2

摘要

根据对东欧地台西南部普里皮亚特-第聂伯岩浆区(普里皮亚特-第聂伯-顿涅茨克岩浆省西北部)岩石学和地球化学研究的结果,结合构造-物质分析的原理,结合前人的研究,首次确定了晚弗拉斯世-早法明世普里皮亚特-第聂伯岩浆区岩石的侧向-时间序列。该系列由四个岩浆活动阶段形成的杂岩组成,按时间间隔分开:Zhlobin杂岩(Rechitsa时间,晚弗拉斯纪开始),Uvarovichi杂岩(晚沃罗涅日时间,晚弗拉斯纪中期),Pripyat杂岩(skolotin - chernin ?)时间,结束了晚期弗拉斯尼(Frasnian)和洛夫(Loev)情结(Yelets- Petrikov?)时间,早期法门纪)。Zhlobin杂岩属于碱性-超镁质(碳酸岩-金伯利岩-钠云母岩)组;Uvarovichi杂岩—碱性基性构造(玄武岩和空纹岩);普里皮亚特杂岩-到碱-镁-盐构造(粗质山岩);洛夫杂岩-到碱性超镁质(霞石)形成。
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The upper devonian magmatic complexes of the South-East Belarus
For the first time, the authors determined lateral-temporal series of magmatic complexes of the Late Frasnian-Early Famennian Pripyat-Dnieper Magmatic Area according to the results of petrological and geochemical study of rocks of the Pripyat-Dnieper Magmatic Area (north-western part of the Pripyat-Dnieper-Donetsk Magmatic Province) in the southwest of the East European Platform using the principles of structural-material analysis and taking into account previous studies. The series consists of four complexes, formed during stages of magmatic activity, separated by time intervals: Zhlobin Complex (Rechitsa Time, the beginning of the Late Frasnian), Uvarovichi complex (Late Voronezh Time, the middle of the Late Frasnian), Pripyat Complex (Skolodin (Skolodin-Chernin?) Time, the end of the Late Frasnian) and Loev complex (Yelets (Yelets- Petrikov?) Time, Early Famennian). The rocks of the Zhlobin Complex belong to the alkaline-ultramafic (carbonatite-kimberlite-nephelinite) formation; Uvarovichi Complex - to the alkaline-mafic formation (basaltoids and phonolites); Pripyat Complex - to the alkaline-mafic-salic formation (trachyandesites); Loev Complex - to the alkaline-ultramafic (nepheline) formation.
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