作为地球动力系统相互作用指标的盐上升形式

IF 0.3 Q4 GEOLOGY
D. S. Zykov, A. V. Poleshchuk, A. O. Agibalov, S. Yu. Kolodyazhny, E. A. Manuilova
{"title":"作为地球动力系统相互作用指标的盐上升形式","authors":"D. S. Zykov, A. V. Poleshchuk, A. O. Agibalov, S. Yu. Kolodyazhny, E. A. Manuilova","doi":"10.3103/s0145875224700200","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>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.</p>","PeriodicalId":44391,"journal":{"name":"Moscow University Geology Bulletin","volume":"26 1","pages":""},"PeriodicalIF":0.3000,"publicationDate":"2024-07-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Forms of Salt Rises as Indicators of Interaction of Geodynamic Systems\",\"authors\":\"D. S. Zykov, A. V. Poleshchuk, A. O. Agibalov, S. Yu. Kolodyazhny, E. A. Manuilova\",\"doi\":\"10.3103/s0145875224700200\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<h3 data-test=\\\"abstract-sub-heading\\\">Abstract</h3><p>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.</p>\",\"PeriodicalId\":44391,\"journal\":{\"name\":\"Moscow University Geology Bulletin\",\"volume\":\"26 1\",\"pages\":\"\"},\"PeriodicalIF\":0.3000,\"publicationDate\":\"2024-07-17\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Moscow University Geology Bulletin\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.3103/s0145875224700200\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Moscow University Geology Bulletin","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3103/s0145875224700200","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

摘要

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。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Forms of Salt Rises as Indicators of Interaction of Geodynamic Systems

Forms of Salt Rises as Indicators of Interaction of Geodynamic Systems

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.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
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.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信