{"title":"corbieres和Minervois(法国)上第四纪构造反转模型的提出。形态和水文后果","authors":"A. Genna, N. Lenôtre, J. Capdeville","doi":"10.1016/S1251-8050(97)82760-7","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":10613,"journal":{"name":"Comptes rendus hebdomadaires des seances de l'Academie des sciences","volume":"27 1","pages":"807-813"},"PeriodicalIF":0.0000,"publicationDate":"1997-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":"{\"title\":\"Proposition d'un modèle d'inversion tectonique au Plio-Quaternaire dans les Corbières et le Minervois (France). Conséquences morphologiques et hydrologiques\",\"authors\":\"A. Genna, N. Lenôtre, J. Capdeville\",\"doi\":\"10.1016/S1251-8050(97)82760-7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":10613,\"journal\":{\"name\":\"Comptes rendus hebdomadaires des seances de l'Academie des sciences\",\"volume\":\"27 1\",\"pages\":\"807-813\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1997-11-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Comptes rendus hebdomadaires des seances de l'Academie des sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1016/S1251-8050(97)82760-7\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Comptes rendus hebdomadaires des seances de l'Academie des sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1016/S1251-8050(97)82760-7","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Proposition d'un modèle d'inversion tectonique au Plio-Quaternaire dans les Corbières et le Minervois (France). Conséquences morphologiques et hydrologiques