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This book describes in detail numerous geological sites throughout the mountains of Oman and the United Arab Emirates (UAE) in Eastern Arabia. The region is well known for its oil and gas reserves in the desert interior, and Permian-Mesozoic shelf carbonates exposed in the mountains of the Musandam peninsula, Jebel al-Akhdar and Saih Hatat, where deep wadi canyons provide impressive three-dimensional views into the crust. The region has numerous globally important geological sites, including the world’s largest and best-exposed ophiolite complex, the Semail Ophiolite, which is a vast thrust sheet of Cretaceous ocean crust and upper mantle emplaced onto the Arabian continental margin. Other sites include spectacular fossil localities, subduction zone metamorphic rocks (eclogites, blueschists, amphibolites), fold-thrust belts, giant sheath folds and Precambrian salt domes, as well as the huge sand dunes of the Rub al’Khali, the Empty Quarter, and the separate Wahiba (Sharkiyah) sandsea of Eastern Oman. Written by Mike Searle, who has worked on geological research projects throughout Oman and UAE almost every year since 1978, this book describes the field geology of each site and includes a wealth of maps, field photos and diagrams illustrating key features. It also discusses the history of exploration of Arabia and the search for its hidden geological secrets. The book provides the geological basis for the establishment of a series of World Heritage Sites, National GeoParks and Sites of Special Scientific Interest (SSSI) throughout the region. As such, it is of interest to geologists, tourists, mountaineers, trekkers, rock climbers and naturalists.
The Oman Mountains contain one of the world’s best- exposed and best-understood fold–thrust belts and the largest, best-exposed and most intensively studied ophiolite complex on Earth. This volume presents new international research from authors currently active in the field focusing on the geology of the Oman Mountains, the foreland region, the carbonate platforms of Northern and Central Oman and the underlying basement complex. In addition there is a particular focus on geoconservation in the region. The volume is divided into three main sections that discuss the tectonics of the Arabian plate using insights from geophysics, petrology, structural geology, geochronology and palaeontology; the petrology and geochemistry of the Oman Ophiolite and the sedimentary and hydrocarbon systems of Oman, drawing on the geophysics, structure and sedimentology of these systems. The volume is enhanced by numerous colour images provided courtesy of Petroleum Development Oman.
Proceedings of an International Discussion Meeting held at the Royal Society of Edinburgh form March 29-31st, 1988, sponsored by the Geological Society of London and Amoco Production Company (International)
The geology of the Oman Mountains, including the Jabal Akhdar and Saih Hatat domes, is extraordinarily well-exposed and diverse, spanning a geological record of more than 800 Ma. The area is blessed with first-class outcrops and is well known in the geological community for its ophiolite. The Oman Mountains have much more to offer; including, Neoproterozoic diamictites (‘Snowball Earth’), fossil-rich Permo–Mesozoic carbonates and metamorphic rocks. The arid climate and deep incision of wadis allow for nearly complete rock exposure which can be investigated in all three dimensions. The diverse geology is also responsible for the breathtaking landscape. New roads and the nature of the friendly Omani people make fieldwork unforgettable. This Memoir provides a thorough state-of-the-art overview of the geology and tectonics of the Southeastern Oman Mountains, and is accompanied by an oversized geological map.
Several important developments in our understanding of the chemistry of weathering have occurred in the last few years: 1. There has been a major breakthrough in our understanding of the mechanisms controlling the kinetics of sil icate dissolution, and there have been major advances in computer modeling of weathering processes. 2. There has been a growing recognition of the importance of organic solutes in the weathering process, and hence of the inter-relationships between mineral weathering and the terrestrial ecosystem. 3. The impact of acid deposition ("acid rain") has been widely recognized. The processes by which acid deposition is neutral ized are closely related to the processes of normal chemical weathering; an understanding of the chemistry of weathering is thus essential for predicting the effects of acid deposition. 4. More high-qual ity data have become available on the chemical dynamics of smal I watersheds and large river systems, which represent the integrated effects of chemical weathering.
The geology of Oman is spectacular - for the touristic layman and the geologist alike. Exceptionally well exposed rocks offer a fascinating outcrop experience, second to none. The scenery is unique, and often breathtaking. The Samail Ophiolite (former sea floor you can walk on), mountain ranges, of more than 3000 m altitude, and deeply incised canyons with turquoise-coloured perennial streams, contrast with dry but golden sand deserts. Coastal areas with kilometres of white beaches are waiting to be discovered. This geological guidebook has two parts: The first provides a general introduction to the geology of Oman, and enables the reader to put the variety of geological phenomena and observations into a scientific context. The authors emphasise describing the processes that led to the formation of Oman's rocks and landscapes formed over millennia of Earth history. Following the introductory chapters on archaeology, climate, and vegetation, the geomorphological and geological aspects of Oman are presented. The second and largest part of the guide consists of meticulous descriptions of 99 excursion points located across the northeast of the country. The challenge in Oman is to decide where not to stop, rather than the other way round. The authors, therefore, have carefully selected the most interesting and important sites. The excursion points can easily be located by their coordinates, or may also be visited using the detailed roadmaps provided for each single outcrop. A large number of colour illustrations, a geological overview map, an index, and a list of references complete the content of the guide. As the book is written in a textbook style and presents the geology in a comprehensible way, a broad understanding is facilitated. Therefore, this field guide not only addresses geologists but also amateurs, visitors and travellers exploring the beauty and the significance of Oman geology.
The 32 papers in this volume examine the mode and nature of igneous, metamorphic, tectonic, sedimentological, and biological processes associated with the evolution of oceanic crust in different tectonic settings in Earth history as revealed in various ophiolites and ophiolite belts around the world, and the geodynamic significance of these ophiolites in the evolution of different orogenic systems. Divided into six thematic sections, the book presents a wealth of new data and syntheses from mainly Phanerozoic ophiolites around the world.
Proceedings of the Ophiolite Conference, held in Muscat, Oman, January 7-18, 1990