首页> 外文期刊>Facies >The bioeroded megasurface of Oura (Algarve, south Portugal): implications for Neogene stratigraphy and tectonic evolution of southwest Iberia: reply to Pais and Legoinha (DOI 10.1007/s10347-011-0268-y)
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The bioeroded megasurface of Oura (Algarve, south Portugal): implications for Neogene stratigraphy and tectonic evolution of southwest Iberia: reply to Pais and Legoinha (DOI 10.1007/s10347-011-0268-y)

机译:欧拉(葡萄牙南部阿尔加维)遭受生物侵蚀的巨型表面:对西南伊比利亚西南地区新近系地层和构造演化的影响:答复佩斯和莱戈尼哈(DOI 10.1007 / s10347-011-0268-y)

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摘要

We start by acknowledging that comments are welcome and the ensuing discussion generally contributes to a better understanding of the scientific questions at stake, in the present case a paleoichnological study of a major Neogene bioeroded surface associated with an ancient rocky shoreline, which may be followed for about 1.5 km along the Oura sea cliffs on central Algarve, in southern Portugal. The aim of Cacha?o et al.’s (2009) paper was to show the geological significance of major bioeroded surfaces, their identification, and interpretation, by demonstrating the importance of the Oura hardground for the understanding of the stratigraphic record of the Neogene of southern Portugal and its correlation with Iberian tectonic development.
机译:我们首先承认欢迎发表评论,随后的讨论通常有助于人们更好地理解所面临的科学问题,在本例中,是对与古代岩石海岸线相关的主要新近系生物侵蚀表面的古生物学研究,可以遵循葡萄牙南部阿尔加维中部的欧拉海崖沿岸约1.5公里。 Cacha?o等人(2009年)的论文旨在通过证明欧拉硬地对于理解新近系地层记录的重要性,来显示主要生物侵蚀表面的地质意义,其识别和解释。葡萄牙南部及其与伊比利亚构造发展的相关性。

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