Forms of Salt Rises as Indicators of Interaction of Geodynamic Systems
IF 0.3
Q4 GEOLOGY
引用次数: 0
Abstract
The forms of salt rises occur under the influence of stresses developing in the Earth’s crust and can therefore be considered sensitive indicators of the interaction of geodynamic systems. The forms of salt rises, reflecting the superposition of these systems, arose in the North German Basin, in the Cis-Uralian Foredeep on the boundary with the Caspian Depression, and in the Pripyat Trough under the influence of various sources of stress and deformation. The mechanisms of such a superposition were both the formation of forms associated with the resulting addition of strain vectors and interference of forms associated with each geodynamic system individually.
作为地球动力系统相互作用指标的盐上升形式
摘要盐隆起是在地壳应力的影响下出现的，因此可被视为地球动力系统相互作用的敏感指标。在各种应力和变形源的影响下，北德盆地、与里海凹陷交界的顺乌拉尔前深海以及普里皮亚季海槽都出现了盐隆起，反映了这些系统的叠加。这种叠加的机制既包括与由此产生的应变矢量相加有关的形式的形成，也包括与每个地球动力系统单独有关的形式的干扰。
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来源期刊
Moscow University Geology Bulletin
GEOLOGY-
CiteScore
0.60
自引率
25.00%
发文量
43
期刊介绍：
Moscow University Geology Bulletin is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.
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