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G.A. Forbes, H.S.M. Jansen and J. Schreurs : Lexicon of Oman: Subsurface Stratigraphy

Gulf Petrol Link, Bahrain, 2010

ISBN 9990110565

4to - over 9¾" - 12" tall. CT2 - A hardcover book in very good condition in very good dust jacket that is mylar protected. Dust jacket has some wrinkling and chipping on the edges and corners, small patch peeled with tiny tear on the back top left corner, some scattered light scratches and rubbing, light tanning and shelf wear. Book has some bumped corners, previous owner's name written on the front free endpaper, some light discoloration and shelf wear. Inclues two (2) folded brochures and CD at the back fixed endpaper pocket. Reference Guide to the Stratigraphy of Oman's Hydrocarbon Bains. GeoArabia Spcial Publications 5, Petroleum Development Oman. 12"x8.5", 371 pages. Satisfaction Guaranteed. Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks. Stratigraphy has two related subfields: lithostratigraphy (lithologic stratigraphy) and biostratigraphy (biologic stratigraphy). The geology of Oman includes varied landscapes which are a blend of its geological history, and its climate over the past few million years. Rock outcrops in Al Hajar Mountains, the Huqf and Dhofar are a point of interest for international geologists. The rock record spans about 825 million years and includes at least three periods when the country was covered by ice. Oman, located at the southeast corner of the Arabian plate, is being pushed slowly northward, as the Red Sea grows wider. The lofty Hajar Mountains and the drowned valleys of Musandam are dramatic reminders of this. Generally speaking Oman is fairly quiescent tectonically. Musandan experiences occasional tremors as the Arabian Plate collides with the Eurasian Plate. During the Cretaceous Period Oman was located adjacent to a subduction zone and a portion of the upper mantle along with overlying seafloor volcanic rocks were thrust over the continental crust. This obducted sequence of ultramafic to mafic rocks is the Semail Ophiolite complex. The ophiolite is locally rich in copper and chromite orebodies. The interior plains of Oman are of young sedimentary rocks, wadi gravels, dune sands and salt flats. Beneath them is a several kilometre-thick stack of older sedimentary rocks that host the country's hydrocarbon resources. Ancient salt, which comes to the surface in several salt domes such as Qarat Kibrit, plays an important role in forming many of these oil and gas accumulations. Oman has become a major destination for geotourism and an increasing number of visitors are attracted by the spectacular outcrops the country has to offer.. Book Condition: Very Good. Binding: Hardcover. Jacket: Very Good

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