By A. Mascle, C. Puigdefabregas, M. Fernandez and H.P. Luterbacher
Presents a latest synthesis on foreland basin series stratigraphy and structural geology. contains the foothills, foreland basins of the Northwestern Alps,Pyrenees and Betic thrust belts. The multidisciplinary strategy contains either sedimentological and structural reports plus numerical modelling as a device to quantify and combine the geological facts. additionally on hand: The Geology of important Europe - quantity 2 Mesozoic and Cenozoic - ISBN 1862392641 The Geology of britain and Wales (Geological Society Geology of sequence GOEWP) - ISBN 978-1-86239-200-7 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on this planet, and one of many greatest publishers within the Earth sciences.The Society publishes a variety of top quality peer-reviewed titles for lecturers and execs operating within the geosciences, and enjoys an enviable overseas acceptance for the standard of its work.The many components during which we post in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reports and geochemistry-Remote sensing-History of geology-Regional geology publications
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Extra resources for Cenozoic Foreland Basins of Western Europe (Geological Society Special Publication No. 134)
In all three wells, the lowermost sediments overlying the autochthonous basement correspond to the 'basal calcarenite' previously recognized by Perconig (1960-62). In the central part of the basin (Fig. 10), the Nueva Carteya-1 well, located on the External Betics, drilled more than 3000 m of Mesozoic carbonates overthrusting THE GUADALQUIVIR BASIN: GEOLOGY & GEOPHYSICS 37 Fig. 8. Location map of subsurface data. Dashed lines indicate the location of seismic profiles used in this study. Solid lines indicate the location of interpreted seismic lines shown in this paper: I (Fig.
MASCLE& C. 1 Ma) -, , ~. . ; -~-~ ~'~ "'""""""'"7 ', B) %. 1 Ma) ..... [ ~. . . . - ' - ' ' - 7 - - - \ . . . ~" .... ~ i ~ i i . ~ - . . . . . . 1 Ma) . " . . . . . ~ D) . . . . . . 5 ~west tilting) pre growth strata dip = 2,5 ~west ~ scanillaFro. 5 km ' H =V INTRODUCTION Nummulites carbonate beds whose lateral continuity goes beyond the syncline-basin itself and can be found in neighbouring basins. Secondorder transgressions are Nummulites and patchreef carbonate beds whose extent is restricted to the syncline basin, but whose lateral equivalents can be traced to overlay the upper delta plain of the underlying sequence.
A A P G Mediterranean Basins Conference, Nice, Field Guide 7. Special Publication of the Institute of Geology, University of Parma, Italy. - - , SGAVETrI,M. & REMACHA,E. 1984. Le relazioni tra piataforme deltizie a sistemi torbiditici nel Bacino Eocenico Sudpirenaico di Tremp-Pamplona. Giornale di Geologia Ser. 3, 46(2), 3-32. NAGTEGAAL, P. J. , VAN VLIET, A. & BROUWER, J. 27 1983. Syntectonic Coastal offlap and Concurrent Turbidite Deposition: the Upper Cretaceous Aren sandstone in the South-Central Pyrenees, Spain.