Download Tracing Tectonic Deformation Using the Sedimentary Record by T McCann and A Saintot PDF
By T McCann and A Saintot
The learn of sediments and sedimentary basins when it comes to their tectonic setting calls for a multidisciplinary technique and has more and more drawn either strategies and pursuits from fields open air sedimentology. the applying of alternative theoretical, experimental and empirical assets supplied by means of structural geology, geochemistry, geophysics, scale modelling, and box geology, supplement sedimentological tools, with the mixed goal of accomplishing a deeper realizing of the origins, evolution and value of sedimentary sequences by way of their tectonic background. reviews offered during this quantity diversity throughout a large spectrum from the research of sedimentary series structure at basin cut down to the chemical houses of person grains, and comprise reviews from quite a number tectonic settings. the quantity may be of curiosity to these concerned with, or considering, reviews regarding the linkages among tectonics and sedimentation, in addition to a much broader viewers to whom the result of such stories could provide clean perception. additionally on hand: Tectonics of the Western Mediterranean and North Africa - ISBN 1862392021 Tectonic improvement of the jap Mediterranean sector: distinctive ebook no 260 - ISBN 186239198X The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on the planet, and one of many biggest 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 acceptance for the standard of its work.The many components during which we submit in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reviews and geochemistry-Remote sensing-History of geology-Regional geology publications
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Extra resources for Tracing Tectonic Deformation Using the Sedimentary Record (Geological Society Special Publication)
Sample text
STARK, C. P. 1991. Sedimentology and tectonic geomorphology adjacent to active and inactive normal faults in the Megara Basin and Alkyonides Gulf, central Greece. Journal of the Geological Society, London, 148, 331-343. LEEDER, M. , HARRIS, T. & KIRKBY, M. J. 1998. Sediment supply and climate change: implications for basin stratigraphy. Basin Research, 10, 7-18. LINDSAY, J. F. & KORSCH, R. J. 1989. Interplay of tectonics and sea-level changes in basin evolution: an example from the intracratonic Amadeus basin, central Australia.
The largest basins are related to the ENE-WSW faults. The rocks of Middle Jurassic age, which predate the faulting stage, are shallow-marine oolitic limestones. The Lower Cretaceous Fardes Formation shows evidence of deposits closer to the carbonate compensation depth (CCD). This evidence indicates that normal faulting was related to very significant thinning of the continental crust. Palaeomagnetic studies in the area demonstrate the existence during the Miocene of clockwise and counterclockwise rotations with vertical axes.
TECTONICS AND SEDIMENTATION IN THE EASTERN BETICS 37 tions (Allerton et al 1994) due to their discon- part of the succession has thick layers of brown tinuous character. This formation consists of sandstones. The overall thickness of the formared and pink limestones and marly limestones tion can reach 500 m. It contains fossils typical of with some turbidite intercalations and slumps shallow-marine environments (Wittink 1975), (Fig. 3). e. deeper marine setting. The base ranges in age deep marine with strong topographic relief and from the Maastrichtian to the Early Eocene, unstable slopes.