由塔古斯河（葡萄牙和西班牙）排水的中小型新生代盆地的形成。地壳褶皱形成的沉积盆地实例

Q4 Earth and Planetary Sciences

Geogaceta Pub Date : 2023-12-18 DOI:10.55407/geogaceta102343

Ramón Vegas

{"title":"由塔古斯河（葡萄牙和西班牙）排水的中小型新生代盆地的形成。地壳褶皱形成的沉积盆地实例","authors":"Ramón Vegas","doi":"10.55407/geogaceta102343","DOIUrl":null,"url":null,"abstract":"The Tagus River drains several small- to medium-sized Cenozoic sedimentary basins situated within a tectonic depression flanked by two basement highs. These basins were formed during the initial stages of the Cenozoic compressive event that affected the interior of the Iberian Peninsula, a consequence of the Africa-Eurasia convergence. These basins exhibit distinct characteristics typical of compressional sedimentary basins, being flanked by thrusts and reverse faults. The mechanism of their formation can be attributed to crustal-scale folds, showcasing a notable and possibly exceptional instance of compressional sedimentary basins created through this tectonic mechanism.","PeriodicalId":37493,"journal":{"name":"Geogaceta","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2023-12-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The formation of small- to medium-sized Cenozoic basins drained by the Tagus river (Portugal and Spain). Example of sedimentary basins formed by crustal-scale folding\",\"authors\":\"Ramón Vegas\",\"doi\":\"10.55407/geogaceta102343\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Tagus River drains several small- to medium-sized Cenozoic sedimentary basins situated within a tectonic depression flanked by two basement highs. These basins were formed during the initial stages of the Cenozoic compressive event that affected the interior of the Iberian Peninsula, a consequence of the Africa-Eurasia convergence. These basins exhibit distinct characteristics typical of compressional sedimentary basins, being flanked by thrusts and reverse faults. The mechanism of their formation can be attributed to crustal-scale folds, showcasing a notable and possibly exceptional instance of compressional sedimentary basins created through this tectonic mechanism.\",\"PeriodicalId\":37493,\"journal\":{\"name\":\"Geogaceta\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-12-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geogaceta\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.55407/geogaceta102343\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geogaceta","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.55407/geogaceta102343","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}

引用次数: 0

摘要

塔古斯河（Tagus River）流经几个中小型新生代沉积盆地，这些盆地位于两个基底高地两侧的构造洼地内。这些盆地形成于新生代压缩事件的初期阶段，该事件影响了伊比利亚半岛内部，是非洲-欧亚大陆汇聚的结果。这些盆地具有典型的压缩沉积盆地的明显特征，两侧有推力断层和逆断层。其形成机制可归因于地壳尺度的褶皱，展示了通过这种构造机制形成的压缩沉积盆地的一个显著且可能是特殊的实例。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文本刊更多论文

The formation of small- to medium-sized Cenozoic basins drained by the Tagus river (Portugal and Spain). Example of sedimentary basins formed by crustal-scale folding

The Tagus River drains several small- to medium-sized Cenozoic sedimentary basins situated within a tectonic depression flanked by two basement highs. These basins were formed during the initial stages of the Cenozoic compressive event that affected the interior of the Iberian Peninsula, a consequence of the Africa-Eurasia convergence. These basins exhibit distinct characteristics typical of compressional sedimentary basins, being flanked by thrusts and reverse faults. The mechanism of their formation can be attributed to crustal-scale folds, showcasing a notable and possibly exceptional instance of compressional sedimentary basins created through this tectonic mechanism.

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

Geogaceta Earth and Planetary Sciences-Geology

CiteScore

0.40

自引率

0.00%

发文量

期刊介绍： Geogaceta is a magazine that publishes semiannually the Geological Society of Spain. This society aims to promote, promote, and disseminate knowledge, progress and applications of Geology; , the advice in scientific and educational matters to the institutions and entities that require it and the representation of the scientific interests of the geological community of Spain at international level. Its members have the right to participate in all the activities organized by the Company, to present their candidacy to any of their management positions and to receive free periodical publications of the Company (Geogaceta and Magazine of the Geological Society of Spain).