By A. Mascle, C. Puigdefabregas, M. Fernandez and H.P. Luterbacher
Presents a latest synthesis on foreland basin series stratigraphy and structural geology. comprises 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 facts. additionally on hand: The Geology of valuable 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 biggest publishers within the Earth sciences.The Society publishes quite a lot of top of the range peer-reviewed titles for teachers and pros operating within the geosciences, and enjoys an enviable overseas popularity for the standard of its work.The many parts 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 courses
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Extra info for Cenozoic Foreland Basins of Western Europe (Geological Society Special Publication No. 134)
1986). A pronounced crustal thinning is observed from the Betics to the Alboran Sea. Different seismic profiles acquired near the shoreline (Banda & Ansorge 1980; Medialdea et al. 1986; Barranco et al. 1990) show a crustal thickness of 23-24 km. The crustal structure in the Alboran Sea is poorly constrained, since the only available data come from seismic experiments shot in 1974 (Hatzfeld 1976; Boloix & Hatzfeld 1977) and in 1979 (Surifiach & Vegas 1993) which show that the Moho lies at about 15 km depth in the central part of the basin.
4. Moho depth map. Isolines every i km. Grey thick lines indicate the location of seismic refraction profiles. Fig. 5. Surface heat flow map in mW m -2. Triangles indicate measurements from water exploration wells. Circles indicate indicate measurements from oil exploration wells. Squares indicate sea-floor measurements. THE GUADALQUIVIR BASIN: GEOLOGY & GEOPHYSICS Temperature (~ Temperature (~ 0 28 21 a, . i . , . i 35 , , . i 42 . 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.
1993. Relationships between thrust tectonics and sequence stratigraphy surfaces in foredeeps: model and examples from the Pyrenees (Cretaceous-Eocene, France, Spain). In: WILLIAMS,G. D. & DOBB, A. (eds) Tectonics and Seismic Stratigraphy. Geological Society, Special Publications London, 71, 193-219. , PUIGDEFABREGAS, C. & TAYLOR,A. M. 1994. Sequence Architecture in a Tectonically Active Setting: The Sobrarbe Formation, Ainsa Basin, Spain. In: JOHNSON, S. D. ) High Resolution Sequence Stratigraphy: Innovations and Applications.