| 书目名称 | The Argentina Continental Margin |
| 副标题 | A Potential Paleocli |
| 编辑 | Roberto A. Violante,Cecilia Laprida,Natalia L. Gar |
| 视频video | |
| 概述 | Includes supplementary material: |
| 丛书名称 | SpringerBriefs in Earth System Sciences |
| 图书封面 |  |
| 描述 | The evolution of the Argentina Continental Margin during the Quaternary and the stratigraphic and morphosedimentary configuration responded to climatic variability, oceanographic changes, glacioeustatic fluctuations and tectono-isostatic processes, which began to impact on the margin during previous geological periods. The final modeling of the margin was achieved in the late Miocene, when the interaction between the Antarctic and North Atlantic water-masses favored climatic and oceanographic changes with a profound effect on morphosedimentary features. In the Quaternary, the different regions of the margin distinctly responded to such changes. Whereas in the shelf the main modeling factors were the sea-level fluctuations of glacioeustatic origin and consequent marine-continental stratigraphic records, in the slope (particularly in the sector corresponding to the passive margin) the prevailing effect was the interaction between water-masses and the sea floor, giving origin to contouritic depositional systems accompanied of gravity processes responsible of turbiditic and mass-wasting deposits. Different relationships between contouritic and turbiditic facies respond to distinct comb |
| 出版日期 | Book 2017 |
| 关键词 | Argentina Continental Margin; Contourites; Marine Quaternary; Marine Sedimentary Processes; Sea-level Fl |
| 版次 | 1 |
| doi | https://doi.org/10.1007/978-3-319-04196-4 |
| isbn_softcover | 978-3-319-04195-7 |
| isbn_ebook | 978-3-319-04196-4Series ISSN 2191-589X Series E-ISSN 2191-5903 |
| issn_series | 2191-589X |
| copyright | The Author(s) 2017 |
发表于 2025-3-21 19:12:17
