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首页> 外文期刊>Canadian journal of earth sciences >Landscape evolution in Africa during the Cenozoic and Quaternary-the legacy and limitations of Lester C. King
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Landscape evolution in Africa during the Cenozoic and Quaternary-the legacy and limitations of Lester C. King

机译:新生代和第四纪期间非洲的景观演变-Lester C. King的遗产和局限性

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摘要

African landscape evolution since 66 Ma reflects interactions among parts of the Earth system from the Core to the Biosphere. We stress changes in those interactions in three events that have dominated landscape development: (i) a climatic revolution when the circumpolar current and the East Antarctic ice sheet first formed similar to 37 Ma; (ii) a tectonic revolution at similar to 32 Ma dominated by elevation of similar to 30 topographic structural swells continent-wide; and (iii) a second climatic revolution in a Northern Hemisphere cooling event (at similar to 2.7 Ma) that triggered Sahara desert initiation and the beginning of glacial cycles in the Northern Hemisphere (similar to 2.15 Ma). We recognize the following distinct features of the great Afro-Arabian continent (similar to 40 M km(2)) that show its relationship to Earth structure and processes: deep mantle structure and dynamics, plate motion with respect to that structure, especially plate-arrest (similar to 32 Ma). The topographic, erosional, geomorphic, and depositional modifications following that tectonic event were strongly influenced by changes around the continent in oceanic and atmospheric circulation that affected the entire continent. Atmospheric circulation changes since similar to 34 Ma have involved zonal winds, the ITCZ, desert formation and destruction, the evolution of the persistent (since similar to 35 Ma) Antarctic ice sheet, and since similar to 32 Ma of the rapidly cycling Eurasian ice sheets. We explain that a widely supported idea that ancient erosion surfaces have survived at high elevations in Africa is the result of a failure to recognize that the present elevations of the continent's swells are dynamically maintained, but do not display a thermochronological signature because they are young (less than similar to 32 My), so that conduction of heat from shallow convection cells has not yet reached the Earth's surface.(R)
机译:自66 Ma以来的非洲景观演变反映了从核心到生物圈的地球系统各部分之间的相互作用。我们在主导景观发展的三个事件中强调了这些相互作用的变化:(i)一次极地洋流和南极东部冰盖初次形成类似于37 Ma的气候革命; (ii)大约32 Ma的构造旋转,以整个大陆的类似30个地形结构隆起的高程为主; (iii)北半球降温事件的第二次气候革命(大约2.7 Ma),引发了撒哈拉沙漠的起源和北半球冰川周期的开始(大约2.15 Ma)。我们认识到非洲-阿拉伯大洲的以下鲜明特征(类似于40 M km(2))表明了其与地球结构和过程的关系:深幔结构和动力学,相对于该结构的板块运动,特别是板块-逮捕(类似于32 Ma)。构造事件之后的地形,侵蚀,地貌和沉积变化受到大陆周围影响整个大陆的海洋和大气环流变化的强烈影响。大气环流变化是由于类似于34 Ma涉及到纬向风,ITCZ,沙漠形成和破坏,持续的(自类似于35 Ma以来)南极冰盖的演化以及自类似于32 Ma的快速循环的欧亚冰盖以来的变化。 。我们解释说,一个广泛支持的观点认为,古代的侵蚀面已经在非洲的高海拔地区幸存下来了,这是由于未能认识到非洲大陆涌浪的当前海拔高度是动态维持的,但由于它们很年轻而未显示出热年代学特征(小于32 My),因此来自浅对流单元的热传导尚未到达地球表面。

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