首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Le domaine Tariquide (arc de Gibraltar,Espagne et Maroc) : succession sédimentaire et événements structuraux au Lias et au Dogger
Authors:Michel Durand-Delga  Silvia Gardin  Manuel Esteras  Hélène Paquet
Institution:1. La Pélisserie, 81150 Florentin, France;2. UMR CNRS 5143, université Pierre-et-Marie-Curie, case 117, 4, place Jussieu, 75252 Paris cedex 05, France;3. SECEG, 3 Estébanez Calderón, 28020 Madrid, Espagne;4. Centre de géochimie de la surface, EOST, CNRS/université Louis-Pasteur, 1, rue Blessig, 67084 Strasbourg cedex, France
Abstract:The Lias–Dogger successions of the Tariquide units in the Gibraltar Arc differ from the series of tectonically adjacent units, the Penibetic (Iberia margin) and the Limestone ‘Dorsale’ (Alboran Domain). Lower Lias limestones are eroded and covered by the Domerian, which starts by deposits of open sea, continuous up to the Dogger (J. Musa-type successions), and elsewhere (Los Pastores-type successions) by a thin series (Upper Lias to Upper Dogger), starting by a manganesiferous episode (Ras Leona) and including marls deposited into three episodes, dated by calcareous nannofossils. Faulting events occurred before the Domerian and during the Late Toarcian (Los Pastores). To cite this article: M. Durand-Delga et al., C. R. Geoscience 337 (2005).
Keywords:Tariquides  Arc de Gibraltar  Los Pastores  Jebel Moussa  Lias  Dogger  Nannoplancton  Manganèse  Tariquides  Gibraltar Arc  Los Pastores  Jebel Musa  Lias  Dogger  Nannoplankton  Manganese
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号