黑海坳陷的构造位置、地质构造及发育特征

I. Lomakin, Ye.A. Sarvirov, V. Kochelab
{"title":"黑海坳陷的构造位置、地质构造及发育特征","authors":"I. Lomakin, Ye.A. Sarvirov, V. Kochelab","doi":"10.15407/gpimo2023.01.033","DOIUrl":null,"url":null,"abstract":"The structural position of the Black Sea deep-sea depression is generally determined by its location in the area of intersection of diagonal transcontinental tectonolineament belts. The different thickness of deposits of the same age in different depressions emphasizes the bloc structure of the earth's crust in the water area. Space photographs clearly show the contours of the depression are enveloping by the long arcs of the mountain ranges and valleys of the Caucasus, Ajaro-Trialetia, and the Eastern and Western Pontides. Such large oval and arcuate, partially sequentially superimposed structures (the Miesian plate, Pannonian and Bohemian massifs) are characteristic of the entire southeastern border of the East European platform and reflect the activity of the processes of destruction of its southern foreland in the zone of development of the classic geosyncline. The available data allow us to assume the superimposed nature of the Black Sea depression, formed as a result of mainly vertical tectonic movements in the field of development of mantle plume activations.","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":"1 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Structural position and some features of the geological structure and the development of the Black Sea Depression\",\"authors\":\"I. Lomakin, Ye.A. Sarvirov, V. Kochelab\",\"doi\":\"10.15407/gpimo2023.01.033\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The structural position of the Black Sea deep-sea depression is generally determined by its location in the area of intersection of diagonal transcontinental tectonolineament belts. The different thickness of deposits of the same age in different depressions emphasizes the bloc structure of the earth's crust in the water area. Space photographs clearly show the contours of the depression are enveloping by the long arcs of the mountain ranges and valleys of the Caucasus, Ajaro-Trialetia, and the Eastern and Western Pontides. Such large oval and arcuate, partially sequentially superimposed structures (the Miesian plate, Pannonian and Bohemian massifs) are characteristic of the entire southeastern border of the East European platform and reflect the activity of the processes of destruction of its southern foreland in the zone of development of the classic geosyncline. The available data allow us to assume the superimposed nature of the Black Sea depression, formed as a result of mainly vertical tectonic movements in the field of development of mantle plume activations.\",\"PeriodicalId\":33769,\"journal\":{\"name\":\"Geologiia i poleznye iskopaemye mirovogo okeana\",\"volume\":\"1 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geologiia i poleznye iskopaemye mirovogo okeana\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.15407/gpimo2023.01.033\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geologiia i poleznye iskopaemye mirovogo okeana","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15407/gpimo2023.01.033","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

摘要

黑海深海坳陷的构造位置一般是由其位于跨大陆对角线构造叠合带的交点区域来确定的。不同凹陷同一年代沉积物厚度的不同,强调了水域地壳的块体结构。太空照片清楚地显示,洼地的轮廓被高加索山脉、阿扎罗-特里亚利亚山脉和山谷的长弧线所包围。这种巨大的椭圆形和弧形部分序贯叠加构造(密斯板块、潘诺尼亚地块和波西米亚地块)是整个东欧地台东南边界的特征,反映了其南部前陆在经典地槽发育区内的破坏活动。现有的资料使我们能够假设黑海坳陷的叠加性质,主要是由于地幔柱活化发展领域的垂直构造运动而形成的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
Structural position and some features of the geological structure and the development of the Black Sea Depression
The structural position of the Black Sea deep-sea depression is generally determined by its location in the area of intersection of diagonal transcontinental tectonolineament belts. The different thickness of deposits of the same age in different depressions emphasizes the bloc structure of the earth's crust in the water area. Space photographs clearly show the contours of the depression are enveloping by the long arcs of the mountain ranges and valleys of the Caucasus, Ajaro-Trialetia, and the Eastern and Western Pontides. Such large oval and arcuate, partially sequentially superimposed structures (the Miesian plate, Pannonian and Bohemian massifs) are characteristic of the entire southeastern border of the East European platform and reflect the activity of the processes of destruction of its southern foreland in the zone of development of the classic geosyncline. The available data allow us to assume the superimposed nature of the Black Sea depression, formed as a result of mainly vertical tectonic movements in the field of development of mantle plume activations.
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
自引率
0.00%
发文量
7
审稿时长
6 weeks
期刊最新文献
State of the geoecosystem of the Dniester Estuary as a component of the geoecotone «Black Sea—Land» Objects of Antique and Medieval Cultural Heritage as a resource of the geoecosystems of the Northern Black Sea Coast and of the Black Sea Shelf in the area of the Bug Estuary Structural position and some features of the geological structure and the development of the Black Sea Depression Design of equipment for observing the distribution of plastic waste in surf zones U-Pb age of titanite from diorit of Osnytsky Block (Volyn Megablock of Ukrainian Shield)
×
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
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 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 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1