首页> 外文期刊>Quaternary International >Landform analysis of the Pueyrredon Lake area in northwestern Santa Cruz, Argentina
【24h】

Landform analysis of the Pueyrredon Lake area in northwestern Santa Cruz, Argentina

机译:阿根廷圣克鲁斯西北部Pueyrredon湖地区的地貌分析

获取原文
获取原文并翻译 | 示例
       

摘要

The aim of this research was to analyze the landforms around Pueyrredon Lake (NW Santa Cruz in Argentina) to contribute to the understanding of the paleoenvironmental evolution of Patagonia during the Late Pleistocene-Early Holocene. The Pueyrredon Lake area belongs to the Patagonian shield, northwest of the Santa Cruz Province (47°22'28" S-71°55'34" W). Characteristic landforms were identified through satellite images (Landsat 7 ETM) and field work. These landforms include glacial troughs, glacier striations and groove casts, three fan deltas on the south margin of Pueyrredon Lake, lacustrine and glacio-lacustrine sediment, and till deposits. In addition, short detailed stratigraphic logs were measured for paleoenvironmental analysis, and several sedimentary deposits were sampled to characterize grain size variations. All of the information is displayed on a geomorphological map. The modern and ancient landforms were also analyzed based on their topographic characteristics, which were determined by a digital elevation model (DEM). Geomorphological conditions of the erosional and depositional processes in the paleoglacial environment were analyzed using longitudinal- and cross-sections. The results shed light on the climatic variability during the most recent geological period. Major changes in the landscape morphology were associated with glacier evolution and the development and division of the great lakes in the eastern Andes, in Central Patagonia.
机译:这项研究的目的是分析Pueyrredon湖(阿根廷西北圣克鲁斯)周围的地貌,以有助于了解晚更新世-早全新世期间巴塔哥尼亚的古环境演变。 Pueyrredon湖地区属于圣克鲁斯省西北部(西纬47°22'28“ S-71°55'34”)的巴塔哥尼亚盾。通过卫星图像(Landsat 7 ETM)和野外工作确定了特征性地形。这些地貌包括冰川槽,冰川条纹和沟槽型铸件,Pueyrredon湖南缘的三个扇三角洲,湖相和冰川湖相沉积物,直至沉积物。此外,还测量了简短的详细地层测井记录,以进行古环境分析,并对一些沉积物进行了采样,以表征粒度变化。所有信息都显示在地貌图上。还根据地形特征分析了现代和古代地形,这些地形特征是由数字高程模型(DEM)确定的。使用纵向和横截面分析了古冰川环境中侵蚀和沉积过程的地貌条件。结果揭示了最近地质时期的气候变化。景观形态的重大变化与冰川演化以及巴塔哥尼亚中部东部安第斯山脉的大湖的发展和分化有关。

著录项

  • 来源
    《Quaternary International》 |2013年第13期|19-33|共15页
  • 作者单位

    Universidad National de La Rioja, Av. Luis M. de fa Fuente S/N, Aplicadas, La Rioja CP 5300, Argentina,Instituto Superior de Estudios Sociales (ISES-CONICET), Argentina;

    Universidad National de Tucuman, Facultad de Cienaas Naturales e I.M.L, Miguel Lillo 205, CP 4000 Tucuman, Argentina;

    Universidad National de Tucuman, Facultad de Cienaas Naturales e I.M.L, Miguel Lillo 205, CP 4000 Tucuman, Argentina;

    Instituto Superior de Estudios Sociales (ISES-CONICET), Argentina,Universidad National de Tucuman, Facultad de Cienaas Naturales e I.M.L, Miguel Lillo 205, CP 4000 Tucuman, Argentina;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号