“欧洲地貌”和未来地貌学范式(以乌克兰语编写的第一本大陆地貌培训手册的结论)

Oleksandr Komliev
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引用次数: 0

摘要

这篇文章强调有必要编写关于大面积地貌学的培训手册。大陆(其部分)和世界部分地区的地形起伏是区域地貌学的研究对象。作者证实了教科书“欧洲地形”的结构和内容,这是第一本用乌克兰语写的关于大陆地貌学的教科书。该手册由引言、两章、结论和参考文献组成。该手册使用6张示意图,9张数字地图,2张表格,28张彩色照片。手册的第一部分专门讨论行星地貌学问题-地球地形的主要规律。土工结构、形态结构和形态雕刻是它们的分类,被认为是它们大小成因分类的一部分,并给出了其关键评价(1.1)。在1.2中,考虑了在最大的地质构造- -大陆脊和海洋洼地- -水平上地球地形的行星特征(形成时间和地球演化过程中的主要趋势)- -海洋面积的增加以大陆面积的减少为代价;地球地质演化过程中地壳主要类型出现的先后顺序;地球岩石圈地质演化格局:海洋型地壳>过渡型地壳>大陆地壳)。1.3 .被认为是地球发育的地貌阶段(古生代末期开始-中生代开始-盘古大陆分裂),在此期间形成了现代地形的主要特征。其特点是:海洋化(通过古台地的破坏使海洋洼地扩大和加深);由于年轻台地(板块)的结合,大陆面积增加;大陆的构造活化(表地造山和重生山的形成)。1.4论述了地球地貌的一般规律——平原台地区、山地(造山带)区、高台地区和复活山的14种主要地貌类型,陆地地貌发育的时代和历史,新构造阶段的作用,研究走向面和水文盆地在地貌研究中的重要性。考虑了地球现代地带性和古地带性形态雕刻的一般规律,以及后者对现代地带性形态雕刻类型发展的影响(1.5)。第二部分由总论和区域论两部分组成。总论部分论述了欧洲的土工结构、形态构造和形态雕刻的主要规律。在区域部分,考虑了作者公认的欧洲(4个区,13个国家)地貌分区分类单位的现代和古代地貌形成。在结论中,作者利用地质学、地貌学、行星学的数据,充实了他认为未来地貌学范式的内容。关键词:欧洲浮雕;地理构造;形态结构;刻蚀地貌;morphochronodynamic概念;地球的热力学演化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
“THE RELIEF OF EUROPE” AND THE PARADIGM OF GEOMORPHOLOGY OF THE FUTURE (CONCLUSIONS TO THE FIRST TRAINING MANUAL ON THE RELIEF OF CONTINENTS WRITTEN IN THE UKRAINIAN LANGUAGE)
The article emphasizes the need to prepare training manuals on the geomorphology of large land areas. The relief of continents (their parts) and parts of the world is an object of regional geomorphology. The author substantiates the structure and content of the textbook "The relief of Europe", the first written in Ukrainian on the geomorphology of the continents. The manual consists of an introduction, 2 chapters, conclusions and a list of references. The manual uses 6 schematic maps, 9 digital maps, 2 tables, and 28 color photos. The first section of the manual is devoted to issues of planetary geomorphology – the main regularities of Earth's relief forms. Geotexture, morphostructure and morphosculpture are the categories of their are considered as parts of their size-genetic classification and its critical assessment is given (1.1). In 1.2 the planetary features of the Earth's relief at the level of the largest geotextures – continental ridges and ocean depressions are considered (the time of formation and the main trends in the process of the Earth's evolution - the increase in the area of the oceans at the expense of the continents; the sequence of the appearance of the main types of the Earth's crust in the process of the geological evolution of the Earth; the scheme of the geological evolution of the Earth's lithosphere: oceanic-type crust > transition-type crust > continental crust). In 1.3 the considered geomorphological stage of the Earth's development (the beginning of the end of the Paleozoic – the beginning of the Mesozoic – the breakup of Pangea), during which the main features of the modern relief were formed. It is characterized by the following trends: oceanization (expansion and deepening of ocean depressions through the destruction of ancient platforms; increasing the area of continents due to the joining of young platforms (plates); tectonic activation of continents (epiplatform orogeny and the formation of reborn mountains). In 1.4 general regularities of the Earth's morphostructure are considered – 14 types of main morphostructures of plain-platform areas, mountain (orogenic) areas, high platforms and revived mountains, the age and history of the development of land morphostructures, the role of the neotectonic stage, the importance of studying alignment surfaces and hydrographic basins in the study of morphostructure. General regularities of the morphosculpture of the Earth – modern zonal and ancient and the influence of the latter on the development of modern, azonal types of morphosculpture are considered (1.5). The second section consists of general and regional parts. The main regularities of geotexture, morphostructure and morphosculpture of Europe are considered in the general part. In the regional part, modern and ancient geomorphological formations of the author's accepted taxonomic units of geomorphological zoning of Europe (4 zones and 13 countries) are considered. In the conclusions, the author, using data from geology, geomorphology, planetology, substantiates, in his opinion, the content of the future paradigm of geomorphology. Key words: relief of Europe, geotecture; morphostructure; morphosculpture; morphochronodynamic concept; thermodynamic evolution of the Earth.
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