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This volume combines original data from the offshore and onshore Levant in various fields like sedimentology, palaeontology, geochemistry, structural geology and geophysics. This multidisciplinary approach provides an overview of the development of the Levant Basin and allows discussion of the later geological history and deformation processes of the Levant provinces
Quaternary of the Levant presents up-to-date research achievements from a region that displays unique interactions between the climate, the environment and human evolution. Focusing on southeast Turkey, Lebanon, Syria, Jordan and Israel, it brings together over eighty contributions from leading researchers to review 2.5 million years of environmental change and human cultural evolution. Information from prehistoric sites and palaeoanthropological studies contributing to our understanding of 'out of Africa' migrations, Neanderthals, cultures of modern humans, and the origins of agriculture are assessed within the context of glacial-interglacial cycles, marine isotope cycles, plate tectonics, geochronology, geomorphology, palaeoecology and genetics. Complemented by overview summaries that draw together the findings of each chapter, the resulting coverage is wide-ranging and cohesive. The cross-disciplinary nature of the volume makes it an invaluable resource for academics and advanced students of Quaternary science and human prehistory, as well as being an important reference for archaeologists working in the region.
Anatolia and the easternmost Mediterranean region, especially Turkey, Cyprus and northern Syria, represent an excellent natural laboratory for the study of fundamental geological processes (e.g. rifting, seafloor spreading, ophiolite genesis and emplacement, subduction, exhumation and collision). Their interaction has created an intriguing array of deep-sea basins, microcontinents and suture zones.The volume's 22 papers include a large amount of new field-based information (much of it multidisciplinary and the product of teamwork). After an overview, the volume is divided into four sections: Late Palaeozoic--Early Cenozoic of the Pontides (northern Turkey); Late Palaeozoic--Early Cenozoic of the Taurides--Anatolides (central and southern Turkey); Late Cretaceous--Pliocene sedimentary basins and structural development (central Anatolia to the Mediterranean); Late Miocene--Recent Neotectonics (southern Turkey, Cyprus and northern Syria). The volume will interest numerous academic researchers, those concerned with resources (e.g. hydrocarbons; mineral deposits) and also hazards (e.g. earthquakes), as well as advanced undergraduate and postgraduate students -- P. 4 of cover.
Over eighty contributions from leading researchers review 2.5 million years of environmental change and human cultural evolution in the Levant.
We are increasingly faced with environmental problems and required to make important decisions. In many cases an understanding of one or more geologic processes is essential to finding the appropriate solution. Earth and Environmental Sciences are by their very nature a dynamic field in which new issues continue to arise and old ones often evolve. The principal aim of this book is to present the reader with a broad overview of Earth and Environmental Sciences. Hopefully, this recent research will provide the reader with a useful foundation for discussing and evaluating specific environmental issues, as well as for developing ideas for problem solving. The book has been divided into nine sections; Geology, Geochemistry, Seismology, Hydrology, Hydrogeology, Mineralogy, Soil, Remote Sensing and Environmental Sciences.
This book focuses on the evolution of sedimentary basins of the Arabian Plate and its surroundings. Because these sedimentary basins developed in various tectonic settings, from extensional or transtensional to flexural, transpressional or compressional, their sedimentary sequences provide unique records of the regional geology. Georesources of the Arabian Plate are also described here, including petroleum potential, reservoirs, water resources, fresh water and deep saline aquifers, as well as materials and ore deposits. The book is made by a set of papers authored by geoscientists working in both academia and industry. Numerous chapters describe some regional important geologic features and selected sedimentary basins from the Middle East, North Africa and the Arabian Peninsula domains. Other chapters focus on georesources. A particular focus is given to the geology of Saudi Arabia. This book is an important contribution to the geology of the Arabian Peninsula and its surroundings. In view of the strategic and economic importance of the regional geology and georesources of the Arabian Plate and Surroundings, this volume will constitute an important reference for a wide range of geoscientists interested in the geology of this region, especially those active in petroleum geosciences and related industry. Ultimately, readers will discover important thematic maps in this book.
Forty-five years after the synthesis of the plate tectonic hypothesis, much newer and better information has been gathered by the seagoers of the world. Contrary to popular opinion among earth scientists, the purveyors of plate tectonics are the present-day snake oil salesmen. This null hypothesis is fraught with misinformation and misconceptions. It is in need of a massive make-over. Midocean ridge spreading does not occur universally, especially in Iceland and the North Pacific basin. Deep earthquakes do not define a descending slab; in fact, do not even occur in most places along the trenches. Therefore, subduction does not occur. Continental drift is a figment of overly active imaginations, and Gondwana is an even greater figment. India has been in place for several billion years rather than wandering around. Index fossils like Lystrosaurus and Cynognathus are misused, misdated, and show nothing. Land bridges have surfaced and been submerged many times over the years allowing for free passage of fauna and flora. Fracture zones, rather than showing the direction of seafloor spreading, leave nothing more than a pattern of at least four different directions on the ocean floor as they intersect in a random fashion. The Chicxulub crater is not the result of a bolide strike, and this was known from the get-go. In 2004 the first edition of Tectonic Globaloney was published. Since that time much new information has been gathered and published. The Ocean Drilling Program has gone defunct as the owners of that program finally realized/admitted that they were not recovering basement material, self-admitting that only eight off-ridge cores had ever reached real basement. Therefore, the age of the ocean floor was unknown and the magnetic anomalies are not ground-truthed. The time has come for the field hands to take over and replace the ideas mostly derived by the geophysicists. Plate tectonics does not work.