By A. Mascle, C. Puigdefabregas, M. Fernandez and H.P. Luterbacher
Offers 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 procedure contains either sedimentological and structural reports plus numerical modelling as a device to quantify and combine the geological info. additionally to be had: The Geology of relevant 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 quite a lot of top quality peer-reviewed titles for lecturers and execs operating within the geosciences, and enjoys an enviable foreign recognition for the standard of its work.The many parts during which we submit in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic stories and geochemistry-Remote sensing-History of geology-Regional geology courses
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Extra info for Cenozoic Foreland Basins of Western Europe (Geological Society Special Publication No. 134)
This convergence, however, is not directly reflected in the kinematics either of the surrounding mountain chains or in the extension of the Alboran basin. In fact, the present-day Guadalquivir basin correlates only with the later steps (Miocene-Recent) of this tectonic history that developed from Late Cretaceous times. Regional geophysical data During the last years several geophysical surveys have been carried out along the southern margin of the Iberian Peninsula. These surveys include deep seismic refraction, wide-angle and reflection profiles, gravity and heat flow.
C: *" 500 ~'250 (D a 35 a 600 1 300 -1 7OO I ! 350 8OO 400 a 9OO I -15 ' ' I 0 ' ' I 15 ' ' I 30 ' ' I ' 45 ' I 60 Gradient (mK m -1) ' ' 450 ' ' ' I 0 ' ' ' b) I 40 ' ' ' I 80 ' ' ' I ' 120 ' ' I 160 Gradient (mK m -1) Fig. 6. Thermometric logs recorded in water exploration wells. Dotted line indicates temperature-depth log. Stepped line indicates thermal gradient-depth log. (a) Example of linear temperature log measured at the western part of the Guadalquivir Basin. Only perturbations of short wave-length associated with fractures are evident.
P. 1969. Etude de la zone sud-Pyr~ndenne dans le Massif de Turb6n (Prov. de Huesca Espagne). These 3e cycle. Univ. Toulouse. , VALLES,D. & DORRONSORO, C. 1988. Source rock potential of an Eocene carbonate slope: the Arm~ncies Formation of the Southern Pyrenean Basin, Northeast Spain. American Association of Petroleum Geologists Bulletin, 72,1019. , Mulqoz, J. , TRAVE, A. & SERRA-KIEL,J. Quantifying the kinematics of detachment folds using the 3D geometry: application to the Mediano anticline (Pyrenees, Spain).
Cenozoic Foreland Basins of Western Europe (Geological Society Special Publication No. 134) by A. Mascle, C. Puigdefabregas, M. Fernandez and H.P. Luterbacher