萨塔普利-茨卡尔图博灰岩地块地貌特征

Tsikarishvili Kukuri, Lezhava Zaza, Asanidze Lasha, Bolashvili Nana, C. Nino, C. Giorgi
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引用次数: 4

摘要

萨塔普里亚-茨卡尔图博灰岩地块的岩溶和洞穴形成的重要因素之一是该地区的地貌特征,但研究仍然很少。岩溶和洞穴形成受地质构造和构造的制约。在工作过程中,我们使用了已经批准的基础和应用研究方法,包括传统和现代方法体系。我们对研究区进行了详细的地貌和岩溶洞穴勘探,开展了大规模的调查工作,在此基础上编制了茨卡尔图博灰岩地块地貌简图,并对其成因类型进行了甄别
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geomorphologic Features of Sataplia-Tskaltubo Limestone Massif
One of the important factors of karsto- and speleogenezis of Sataplia-Tskaltubo limestone massif is a still poorly studied geomorphological peculiarity of the region. Karsto- and speleogenezis is conditioned by the geological structure and tectonics. In the working process we used the already approved fundamental and applied research methods, both traditional and modern method systems. We carried out the detailed geomorphologic and karst-speleological exploration of the research area, conducted a large-scale survey works, on the basis of which we compiled the geomorphologic schematic map of Tskaltubo limestone massif and singled out the relief’s genetic types
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