Titlebook: Arabian Plate and Surroundings:Geology, Sedimentary Basins and Georesources; Sami Khomsi,Fran?ois M. Roure,Ammar Amin Book 2020 Springer N

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Regional Geology Reviewshttp://image.papertrans.cn/b/image/160578.jpg

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Filibuster

https://doi.org/10.1007/978-1-4899-0044-9”. The formation commonly consists of sandstones with some claystones, shales, lignites and locally volcanic rocks. Based on outcrop samples taken in the central and northern parts of Mount Lebanon the petrographical composition of the typical Chouf Sandstone is dominated by monocrystalline quartz (

cogent

Visual-Acuity

https://doi.org/10.1007/978-1-4757-9528-8rphology to constrain relief evolution in a rift setting from a high-resolution database at basin-scale (~300?km?×?100?km) including, digital elevation model, outcrop and subsurface data. The stratigraphic architecture shows five main stages ranging from rift initiation to tectonic quiescence (Oligo

肉身

https://doi.org/10.1007/978-3-663-07212-6Atlas front in Tunisia. The Northern Chotts Range, one of most geologic features in southern Atlas, separates a dominantly deformed area of Gafsa to the north, from a relatively undeformed area of Chotts basin and Saharan platform to the south. The Cenozoic contractional period shapes a chain with m