By Pierre-Charles de Graciansky, David G. Roberts, Pierre Tricart
The target of the ebook is to supply an up-to-date synthesis of the evolution of the Alpine fold belt hitherto no longer on hand in English. the general suggestion is to construct on classical Alpine geological experiences made because the commence of the nineteenth century by way of integrating this paintings with sleek effects received systematically on mid ocean ridges and passive margins world wide during the last 50 years utilizing new marine geological and geophysical applied sciences. The booklet hence offers an built-in evaluate of the evolution of the Alps from rift to passive margin to the current fold belt over a time span of 300my.* an built-in multidisciplinary synthesis of the evolution of the Alps from rift to passive margin to foldbelt. * one hundred seventy five figures, structural maps and move sections. * an index of localities mentioned within the fext and figures. * a quick precis of the background and improvement of rules about the evolution of fold belts and passive margins because the nineteenth century. * presents foundation for additional enquire and study * presents wider context appropriate to marine and oil geoscientists.
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Additional resources for The Western Alps, from Rift to Passive Margin to Orogenic Belt
Example text
Simplified after McKenzie (1978). (B) Model of simple shear applied to the whole continental crust and mantle generalized from observations in the Basin and Range province (Western USA). Simplified after B. Wernicke (1985). (C) A more recent model also proposes simple shear. Extension is largely done by delamination along the surfaces of discontinuity between ductile and brittle layers. This model is probably more realistic in terms of rheology. Simplified after Lister, Etheridge and Simon (1991) Scheme A has allowed modelling of the subsidence and heat flow in rifts and newly formed margins.
This cordillera was identified as an ‘embryonic nappe’. Ophiolites were supposed to have been injected at the base of the internal cordillera, which formed another ‘embryonic nappe’. The idea of ‘embryotectonic’ interpretation comes from the Swiss author Argand (1916). In Lemoine (1988). (C) Tentative palinspastic reconstructions across the palaeogeographic domains of the Western Alps, after Lemoine (1975). These sections are taken from the foundation paper that is one of the first up-to-date interpretations of the Western Alps in Mesozoic time.
Reproduced after M. Lemoine (1975), Fig. 2, p. 211. 10 The Western Alps, from Rift to Passive Margin to Orogenic Belt basins and that the underlying crust must be very thin. He also inferred a large pressure differential between continents and oceans would be a consequence of this variation speculating that this might cause the step faulting observed on the coastal segments of margins such as South Africa and eastern South America. Laborious measurements of gravity in submarines by Meinesz among others resulted in the conclusion that the cause of the gravity variation was abrupt thinning of the sialic continental crust across the continental margin.