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A publication of the Mediterranean Consortium for the 32nd International Geological Congress
Adopting a global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys and Eurasian plates over the last 600 Ma of Earth’s history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic, which was succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; and the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have increasingly attracted international interest in exploring the geology of the Iberian Peninsula. This final volume of the Geology of Iberia focuses on the active geological processes in Iberia including seismicity and active faulting as well as the modern landscapes in the Iberian Peninsula.
This richly illustrated book provides an overview of the Neoproterozoic Pan-African Belt of Egypt (PABE), which represents the northwestern continuation of the Arabian-Nubian Shield (ANS) and the East African Orogen (EAO). The first chapter offers an introduction to the Turin Papyrus Map and the historical background of the PABE, while the second addresses how the PABE is related to the ANS and EAO. Rock succession of the PABE is dealt with in Chapter 3, while Chapter 4 focuses on Sinai Metamorphic Core Complexes and implications on the break-up of Rodinia. Subsequent chapters discuss a broad range of topics, e.g. ophiolite-dominated suprastructural rocks; volcanosedimentary succession, Neop...
This collection of essays highlights cultural features and processes which characterized translation practice under the dictatorships of Benito Mussolini (1922-1940) and Francisco Franco (1939-1975). In spite of the different timeline, some similarities and parallelisms may be drawn between the power of the Fascist and the Francoist censorships exerted on the Italian and Spanish publishing and translation policies. Entrusted to European specialists, this collection of articles brings to the fore the “microhistory” that exists behind every publishing proposal, whether collective or individual, to translate a foreign woman writer during those two totalitarian political periods. The nine chapters presented here are not a global study of the history of translation in those black times in contemporary culture, but rather a collection of varied cases, small stories of publishers, collections, translations and translators that, despite many disappointments but with the occasional success, managed to undermine the ideological and literary currents of the dictatorships of Mussolini and Franco.
A publication of the Mediterranean Consortium for the 32nd International Geological Congress
This book provides a multi-scale and multidisciplinary perspective on the geology of Azerbaijan, a country characterized by a unique tectonic and geological setting including the Greater and Lesser Caucasus, the Talysh Mountains, and the Caspian and Kur Basins. Essential geological and geophysical data shed light on the principles of the evolution of the Earth within the region under study, seismic activity and the distribution of economic deposits. Further, special attention is paid to the history of geological-geophysical studies in the region. A combined, comprehensive interpretation of Azerbaijan’s near-surface and deep geological structure is achieved on the basis of an integrative analysis of stratigraphic, magmatic, morphological, lithological, tectonic, neotectonic, geophysical and other data, combining not only Russian and Azerbaijani-published, but also wholly new geological data. Volume I addresses the needs of researchers focused on geology and the environmental sciences, but will also be of interest to anyone looking to learn more about the natural phenomena in Azerbaijan, a beautiful country situated at the boundary between Europe and Asia.
This book summarizes the geomorphology, geology, geochronology, geophysics and mineral resources of the Congo Basin, one of the world’s most enigmatic and poorly understood major intra-continental sedimentary basins, and its flanking areas of Central Africa. It provides an up to date analysis of the large region’s origin and evolution. The book’s nineteen chapters take the reader through the entire basement history, as well as the Basin’s ca. 700 million years of cover sequences. Starting from its Archean cratons and Proterozoic mobile belts, and proceeding through the Phanerozoic sequences, including the most recent Cenozoic successions, the book also explores the present drainage s...
This richly illustrated book offers a concise overview of the geology of Egypt in the context of the geology of the Arab Region and Northeast Africa. An introductory chapter on history of geological research in Egypt sheds much light on the stages before and after the establishment of Egyptian Geological Survey (the second oldest geological survey worldwide), Hume's book and Said's 1962, 1990 books. The book starts with the Precambrian geology of Egypt, in terms of lithostratigraphy and classifications, structural and tectonic framework, crustal evolution and metamorphic belts. A dedicated chapter discusses the Paleozoic-Mesozoic-Cenozoic tectonics and structural evolution of Egypt. A chapter highlights the Red Sea tectonics and the Gulf of Suez and Gulf of Aqaba Rifts. Subsequent chapters address the Phanerozoic geology from Paleozoic to Quaternary. The Egyptian Impact Crater(s) and Meteorites are dealt with in a separate chapter. The Earth resources in Egypt, including metallic and non-metallic ore deposits, hydrocarbon and water resources, are given much more attention throughout four chapters. The last chapter addresses the seismicity, seismotectonics and neotectonics of Egypt.
This book addresses the geology of the entire Himalayan range in Nepal, i.e., from the Gangetic plain in the south to the Tethyan zone in the north. Without a comprehensive look at the various Himalayan zones, it is practically impossible to fully grasp the processes at work behind the formation and development of the spectacular Himalaya. However, the goal is not merely to document all the scientific ontology but rather to reveal a sound basis for the prevailing concepts. Both the early literature on Himalayan geology and contemporary trends are fully covered. For the first time, the origin, use, and abuse of common Himalayan geological terms such as the Siwaliks, Lesser Himalaya, Main Boundary Thrust, Main Central Thrust, and Tethys are discussed. The book will help readers to progress from a cognitive approach to a constructive one by linking various types of knowledge, such as seeking relations between various geological structures as well as between earlier thoughts or views and contemporary approaches.