The Alps, Carpathians and Dinarides form a complex, highly curved and strongly coupled orogenic system. Motions of the European and Adriatic plates gave birth to a number of 'oceans' and microplates that led to several distinct stages of collision. Although the Alps serve as a classical example of collisional orogens, it becomes clearer that substantial questions on their evolution can only be answered in the Carpathians and Dinarides. Our understanding of the geodynamic evolution of the Alpine-Dinaride-Carpathian System has substantially improved and will continue to develop; this is thanks to collaboration between eastern and western Europe, but also due to the application of new methods and the launch of research initiatives. The largely field-based contributions investigate the following subjects: pre-Alpine heritage and Alpine reactivation; Mesozoic palaeogeography and Alpine subduction and collision processes; extrusion tectonics from the Eastern Alps to the Carpathians and the Pannonian Basin; orogen-parallel and orogen-perpendicular extension; record of orogeny in foreland basins; tectonometamorphic evolution; and relations between the Alps, Apennines and Corsica.

This volume addresses the tectonic complexity and diversity of strike-slip restraining and releasing bends with 18 contributions divided into four thematic sections: a topical review of fault bends and their global distribution; bends, sedimentary basins and earthquake hazards; restraining bends, transpressional deformation and basement controls on development; releasing bends, transtensional deformation and fluid flow.

Annotation The objective of the book is to provide an updated synthesis of the evolution of the Alpine fold belt hitherto not available in English. The overall concept is to build on classical Alpine geological studies made since the start of the 19thcentury by integrating this work with modern results obtained systematically on mid ocean ridges and passive margins worldwide over the past 50 years using new marine geological and geophysical technologies. The book thus provides an integrated overview of the evolution of the Alps from rift to passive margin to the present fold belt over a time span of 300my. * an integrated multidisciplinary synthesis of the evolution of the Alps from rift to passive margin to foldbelt. * 175 figures, structural maps and cross sections. * an index of localities referred to in the fext and figures. * a brief summary of the history and development of ideas concerning the evolution of fold belts and passive margins since the 19th century. * provides basis for further enquire and research * provides wider context relevant to marine and oil industry geoscientists.