{"title":"Pérmico continental en España.","authors":"C. Virgili, Amparo Ramos, A. Sopeña, S. Costa","doi":"10.5209/REV_CGIB.1977.V4.2875","DOIUrl":null,"url":null,"abstract":"The present data show that the Spanish Permian is represented by the «Autunian» (Lower Rotliegendes) in a typical grey facies and redbeds similar to the «Saxonian» (Upper Rotliegendes). The Upper Permian has been found only in a very few points. In general it is made of detrital series, from clays to conglomerates; some volcanic levels are found. Tickness is very variable, up to 2.000 meters. Sedimentation takes place in continental basins, tectonically con troled 1w the tardihercynian pbases. Their caracteristics and problenis are similar to the ones of Western European Permian. 1.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"24 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"8","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of iberian geology: an international publication of earth sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5209/REV_CGIB.1977.V4.2875","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 8
Abstract
The present data show that the Spanish Permian is represented by the «Autunian» (Lower Rotliegendes) in a typical grey facies and redbeds similar to the «Saxonian» (Upper Rotliegendes). The Upper Permian has been found only in a very few points. In general it is made of detrital series, from clays to conglomerates; some volcanic levels are found. Tickness is very variable, up to 2.000 meters. Sedimentation takes place in continental basins, tectonically con troled 1w the tardihercynian pbases. Their caracteristics and problenis are similar to the ones of Western European Permian. 1.
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