A. Pérez-Estaún, Dennis Brown, Joaquina Álvarez-Marrón, V. N. Puchkov, R. Carbonell
{"title":"乌拉尔南部的构造演化","authors":"A. Pérez-Estaún, Dennis Brown, Joaquina Álvarez-Marrón, V. N. Puchkov, R. Carbonell","doi":"10.17811/TDG.21.1999.265-283","DOIUrl":null,"url":null,"abstract":"The Urals were formed at the end of the Paleozoic by the accretion of several lithospheric elements. A complete accretionary complex is developed at the collision zone, including: offscraping sediments, an accretionary prism, ophiolitic units and a high pressure belt. Geophysical and geological data suggest that this orogen is preserved since its formation, without evidences of post-orogenic collapse or later reactivations.","PeriodicalId":252745,"journal":{"name":"Trabajos de Geologia","volume":"47 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1999-12-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"La evolución tectónica del Sur de los Urales\",\"authors\":\"A. Pérez-Estaún, Dennis Brown, Joaquina Álvarez-Marrón, V. N. Puchkov, R. Carbonell\",\"doi\":\"10.17811/TDG.21.1999.265-283\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Urals were formed at the end of the Paleozoic by the accretion of several lithospheric elements. A complete accretionary complex is developed at the collision zone, including: offscraping sediments, an accretionary prism, ophiolitic units and a high pressure belt. Geophysical and geological data suggest that this orogen is preserved since its formation, without evidences of post-orogenic collapse or later reactivations.\",\"PeriodicalId\":252745,\"journal\":{\"name\":\"Trabajos de Geologia\",\"volume\":\"47 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1999-12-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Trabajos de Geologia\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.17811/TDG.21.1999.265-283\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Trabajos de Geologia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.17811/TDG.21.1999.265-283","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The Urals were formed at the end of the Paleozoic by the accretion of several lithospheric elements. A complete accretionary complex is developed at the collision zone, including: offscraping sediments, an accretionary prism, ophiolitic units and a high pressure belt. Geophysical and geological data suggest that this orogen is preserved since its formation, without evidences of post-orogenic collapse or later reactivations.
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