喀尔巴阡山脉的索洛维诺洼地地貌发展史

Y. Kravchuk, V. Chalyk
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引用次数: 0

摘要

对地形发展的四个阶段进行了分析,并在Solotvyno空心中形成了相应的综合体。主要关注的是形态结构和形态雕塑特征。第三目和第四目的形态结构是有区别的。在形态雕刻的元素中,主要关注剥蚀和剥蚀堆积面(Kycherska, Skrydeyska, Boronyavska)。对新技术运动在这些地表和河谷形成中的作用进行了评价。上巴登的第二阶段与海盆的退缩和陆地分裂成山脉有关。现代地形的主要特征形成于上新世更新世阶段,是一个具有阶地、剥蚀面和剥蚀堆积面复合的河网,边缘地带有勘探形式。基切尔斯卡剥蚀面年龄为非年龄型。根据孢粉学分析,推测Skrydei剥蚀堆积面年龄为上新世-下更新世。Boronyava表面的年龄被认为是更新世,其冲积物中存在变质岩石的鹅卵石(高达5%)。近代以来,新分化的构造运动更为活跃,侵蚀、滑坡、卤素岩溶等外源作用也更为活跃。关键词:剥蚀与剥蚀积面;古冲积层的力量;现代形态动力学过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
HISTORY OF THE SOLOTVYNO HOLLOW OF TRANSCARPATHIA RELIEF DEVELOPMENT
The analysis of four stages of relief development is done, which created the corresponding complexes within the Solotvyno hollow. The main attention is paid to the morphostructural and morphosculptural features. The morphostructures of the third and fourth orders are distinguished. Among the elements of morphosculpture the main attention is paid to denudation and denudation-accumulative surfaces (Kycherska, Skrydeyska, Boronyavska). The role of the new technological movements in the formation of these surfaces and river valleys was rated. The second stage of the upper baden is associated with the retreat of the sea basin and the division of the land into mountains. The main features of the modern relief were formed in the Pliocene Pleistocene stage - a river network with a complex of terraces, denudation and denudation-accumulative surfaces, quest forms in the marginal zone. Age of the Kicherska denudation surface is pannon-pont. According to the palynological analysis, the estimated age of the Skrydei denudation-accumulative surface is upper pliocene-lower pleistocene. The age of the Boronyava surface is considered to be Eopleistocene, and pebbles of metamorphic rocks are present in its alluvium (up to 5%). In the modern period, newer differentiated tectonic movements have become more active, which have contributed to the active manifestation of exogenous processes: erosion, landslides, and halogen karst. Key words: denudation and denudation-accumulative surfaces; power of ancient alluvium; modern morphodynamic processes.
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