Lithostratigraphy of the “Schist-Greywacke Domain” in Portugal: a reappraisal

Q4 Earth and Planetary Sciences
Carlos De Meireles, P. Castro, N. Vaz, Carlos Ângelo, N. Ferreira, A. Sequeira, A. Sá
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Abstract

A synthesis of the knowledge of the Schist-Greywacke Domain (SGD) in Portugal is here presented. Until recently, this sequence assumed the designation of Dúrico-Beirão Supergroup composed by the Douro Group (DG) and the Beiras Group (BG). The DG is considered of Neoproterozoic – Cambrian age and the BG is of Neoproterozoic age. The identification and mapping in the BG of an unconformity as the Cadomian unconformity identified in Spain, which splits the Neoproterozoic in “lower Alcudian” and “upper Alcudian”, is a turning point for the understanding and establishment of consistent stratigraphic sequences that now compose the Fróia and the Lousã groups assembled in the Beiras Supergroup. These new groups are correlated with the Neoproterozoic sequences currently recognized in Spain: the Lousã group is equivalent to the Ibor Group (upper Alcudian) and the Fróia Group is equivalent pro parte, to the Domo Extremeño Supergroup.  
葡萄牙“片岩-格雷瓦克域”岩石地层学的再评价
本文综合介绍了葡萄牙片岩-格雷瓦克结构域(SGD)的相关知识。直到最近,这个序列被命名为Dúrico-Beirão超群,由Douro群(DG)和Beiras群(BG)组成。DG被认为是新元古代-寒武纪,BG被认为是新元古代。西班牙发现的卡多米尼亚不整合面,将新元古代划分为“下阿尔库德斯”和“上阿尔库德斯”,在BG中发现和绘图,是认识和建立一致地层层序的转折点,这些层序组成了贝拉斯超群中的Fróia和Lousã群。这些新群与目前在西班牙发现的新元古代序列相对应:Lousã群相当于Ibor群(上阿尔库德世),Fróia群相当于Domo Extremeño超群。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Cadernos do Laboratorio Xeoloxico de Laxe
Cadernos do Laboratorio Xeoloxico de Laxe Earth and Planetary Sciences-Earth and Planetary Sciences (all)
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