Nathalie Feuillet, Isabelle Manighetti, Paul Tapponnier
{"title":"垂直于小安的列斯群岛弧线俯冲的主动延伸(瓜德罗普,法属安的列斯群岛)","authors":"Nathalie Feuillet, Isabelle Manighetti, Paul Tapponnier","doi":"10.1016/S1251-8050(01)01543-9","DOIUrl":null,"url":null,"abstract":"<div><p>Active normal faults cut the uplifted reef platforms of Grande-Terre and Marie-Galante and the volcanic rocks of Basse-Terre in the Lesser Antilles arc. New marine geophysical data shows that such faults extend offshore, forming two distinct sets. One set bounds graben perpendicular to the arc, attesting to ∼ north–south extension. The ‘en echelon’ faults of the other set, roughly along the volcanic arc, accommodate a component of sinistral motion. The active Soufrière volcano lies inside the western termination of the Marie-Galante graben. Historical and instrumental earthquakes with magnitude ⩾5.5 may have ruptured the Marie-Galante graben bounding faults.</p></div>","PeriodicalId":100301,"journal":{"name":"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science","volume":"333 9","pages":"Pages 583-590"},"PeriodicalIF":0.0000,"publicationDate":"2001-11-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1251-8050(01)01543-9","citationCount":"46","resultStr":"{\"title\":\"Extension active perpendiculaire à la subduction dans l'arc des Petites Antilles (Guadeloupe, Antilles françaises)\",\"authors\":\"Nathalie Feuillet, Isabelle Manighetti, Paul Tapponnier\",\"doi\":\"10.1016/S1251-8050(01)01543-9\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Active normal faults cut the uplifted reef platforms of Grande-Terre and Marie-Galante and the volcanic rocks of Basse-Terre in the Lesser Antilles arc. New marine geophysical data shows that such faults extend offshore, forming two distinct sets. One set bounds graben perpendicular to the arc, attesting to ∼ north–south extension. The ‘en echelon’ faults of the other set, roughly along the volcanic arc, accommodate a component of sinistral motion. The active Soufrière volcano lies inside the western termination of the Marie-Galante graben. Historical and instrumental earthquakes with magnitude ⩾5.5 may have ruptured the Marie-Galante graben bounding faults.</p></div>\",\"PeriodicalId\":100301,\"journal\":{\"name\":\"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science\",\"volume\":\"333 9\",\"pages\":\"Pages 583-590\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-11-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1251-8050(01)01543-9\",\"citationCount\":\"46\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1251805001015439\",\"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 de l'Académie des Sciences - Series IIA - Earth and Planetary Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1251805001015439","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Extension active perpendiculaire à la subduction dans l'arc des Petites Antilles (Guadeloupe, Antilles françaises)
Active normal faults cut the uplifted reef platforms of Grande-Terre and Marie-Galante and the volcanic rocks of Basse-Terre in the Lesser Antilles arc. New marine geophysical data shows that such faults extend offshore, forming two distinct sets. One set bounds graben perpendicular to the arc, attesting to ∼ north–south extension. The ‘en echelon’ faults of the other set, roughly along the volcanic arc, accommodate a component of sinistral motion. The active Soufrière volcano lies inside the western termination of the Marie-Galante graben. Historical and instrumental earthquakes with magnitude ⩾5.5 may have ruptured the Marie-Galante graben bounding faults.