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Carboniferous glacial erosional and depositional featuresin Argentina

机译:阿根廷的石炭纪冰川侵蚀和沉积特征

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Carboniferous glacial deposits occur in basins scattered along the southern Gondwana margin from southernBolivia to eastern Australia. In this paper we describe a variety of glacigenic erosional and depositional featuresin western Argentina and central Patagonia including striated pavements associated with tillites, channel-fill con-glomerates and linear sand bodies genetically linked to palaeoeskers. We also describe bedrock features previouslyunknown in glacial deposits of this age, including grooved and channeled rock surfaces at different scales thatare thought to represent glacial meltwater-sculpted forms. Collectively, these lines of evidence indicate that thearea of land surface covered with ice during this glacial period was probably as large as it was during the EarlyPermian glacial period.
机译:石炭纪的冰川沉积物发生在从冈比亚南部到澳大利亚东部沿冈瓦纳南部边缘散布的盆地中。在本文中,我们描述了阿根廷西部和巴塔哥尼亚中部的各种成冰作用的侵蚀和沉积特征,包括与岩层相关的横纹路面,通道填充砾岩和与古植物遗传相关的线性砂体。我们还描述了这个时代冰川沉积物中以前未知的基岩特征,包括不同比例的带槽和带槽的岩石表面,被认为代表了冰川融水雕刻的形式。总的来说,这些证据表明,在这个冰川期,被冰覆盖的土地表面面积可能与二叠纪早期冰川期的面积一样大。

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