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Reply to comments by C. Labails and W. Roest on ‘Breakup of Pangaea and plate kinematics of the central Atlantic and Atlas regions’

机译:回复C. Labails和W. Roest关于“ Pangea断裂和大西洋中部和阿特拉斯地区的板块运动学”的评论

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摘要

In their comment, Labails and Roest have raised several points against the kinematic model of Schettino and Turco for the central Atlantic region, which requires the existence of an independent Moroccan Plate during the Oligocene and the early Miocene. We thank these authors for giving us the opportunity to clarify some controversial points, but disagree with most of their objections and show that they are based either on a different interpretation of existing data or a distortion of the facts presented by Schettino and Turco.
机译:Labails和Roest在评论中针对大西洋中部地区Schettino和Turco的运动学模型提出了几点观点,该模型要求在渐新世和中新世早期存在一个独立的摩洛哥板块。我们感谢这些作者给我们提供机会澄清一些有争议的观点,但不同意他们的大多数反对意见,并表明它们要么基于对现有数据的不同解释,要么基于Schettino和Turco提出的事实的歪曲。

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