顿涅茨盆地和顿涅茨-顿涅茨瀑布的地质构造统一性

M.V. Zhikalyak, V. Lukinov, O.H. Tsokha
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引用次数: 0

摘要

在对顿巴斯地区和DDZ东南部前中生代地表进行中尺度填图的基础上,利用地震地层学和重力学工作成果,结合科学研究、文献资料和创新假设的分析,证实了顿巴斯地区和DDZ的地质和大地构造统一性。明确了边缘及其中心部分的地质构造特征,首次识别并绘制了16个东北走向的高山隆起带和隆起带,其中DDZ有5个,Donbass有4个,DDZ和Donbass各有4个。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
GEOLOGICAL AND GEOTECTONIC UNITY OF THE DONETS BASIN AND THE DNIPROV-DONETS FALLS
On the basis of medium-scale mapping of the pre-Mesozoic surface of Donbas and the southeastern part of the DDZ, the use of the results of seismostratigraphic and gravimetric works, the analysis of scientific research, publications and innovative hypotheses, the geological and geotectonic unity of Donbas and the DDZ is substantiated. The features of the geological structure of the fringes and their central part were specified, and 16 alpine uplifts and downlifts of the northeastern trend were identified and mapped for the first time, including 5 drops in DDZ and 4 - in Donbass and 4 drops each to DDZ and Donbass.
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