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Hardbound. During the past two decades the pace of geological work in the Himalayas has considerably increased. Of the different sectors, the Western Himalaya has been studied more extensively than the other parts. A fairly good amount of data on different aspects, viz. stratigraphy, sedimentology, geochemistry, geochronology and structure has been generated from different tectonic zones of Western Himalaya. This book compiles and synthesizes the post-1964 data of the Western Himalaya. The geology of Western Himalaya is described under a tectonic zone framework, and wherever necessary, different regions are discussed separately under each tectonic zone. A geological map of the Western Himalaya has been compiled on 1:1,000,000 scale.
Papers from a symposium held in San Antonio, Texas, 1986. Contributors consider problems of crustal and lithospheric scales in this area. Contains a folded map of the Salt Range, Pakistan. Annotation copyright Book News, Inc. Portland, Or.
First Published in 2004. Routledge is an imprint of Taylor & Francis, an informa company.
The Himalayan mountain belt, which developed during the India–Asia collision starting about 55 Ma ago, is a dramatically active orogen and it is regarded as the classic collisional orogen. It is characterized by an impressively continuous 2500 km of tectonic units, thrusts and normal faults, as well as large volumes of high-grade metamorphic rocks and granites exposed at the surface. This constitutes an invaluable field laboratory, where amazing crustal sections can be observed directly in very deep gorges. It is possible to unravel the tectonic and metamorphic evolution of litho-units, to observe the mechanisms of exhumation of deep-seated rocks and the propagation of the deformation. Himalayan tectonics has been the target of many studies from numerous international researchers over the years. In the last 15 years there has been an explosion of data and theories from both geological and geophysical perspectives. This book presents the results of integrated multidisciplinary studies, including geology, petrology, magmatism, geochemistry, geochronology and geophysics, of the structures and processes affecting the continental lithosphere. These processes and their spatial and temporal evolution have major consequences on the geometry and kinematics of the India–Eurasia collision zone.
The crash of the Indian plate into Asia is the biggest known collision in geological history, and it continues today. The result is the Himalaya and Karakoram - one of the largest mountain ranges on Earth. The Karakoram has half of the world's highest mountains and a reputation as being one of the most remote and savage ranges of all. In this beautifully illustrated book, Mike Searle, a geologist at the University of Oxford and one of the most experienced field geologists of our time, presents a rich account of the geological forces that were involved in creating these mountain ranges. Using his personal accounts of extreme mountaineering and research in the region, he pieces together the geological processes that formed such impressive peaks.
First Published in 2004. Plate tectonic collision, climate oscillation, glacial fluctuation, severe wind and water erosion—all have wrought dramatic change on the landscape of the Western Himalaya, one of the most dynamic and spectacular landscapes on Earth. Study of the region—from the Western Himalaya foothills and lowlands to the Arabian Sea—is of particular value to geology and geomorphology because of the size and frequency of events. That much of South Asia is relatively inaccessible has enhanced the significance of research in Pakistan and adjacent areas. Himalaya to the Sea focuses on the general evolution of landforms in Pakistan but also represents an essential guide for predictive, protective and remedial measures to mitigate the natural hazards which plague the region and constrain development. The book describes regional erosion and sedimentation within the context of topographical evolution; more specifically, chapters deal with neotectonics, past and present glaciation, general mountain geomorphology and process mechanics, past and present fluvial processes and landforms, wind-blown loess deposits, age dates, soils, marine terraces and archaeology. This is the first integrated assessment of the geomorphology and Quaternary evolution of this region, from highlands to ocean. Presenting new research, methodologies and theory, this highly illustrated volume also provides the first comprehensive bibliography to the region.