P. H. Liotta, James F. Miskel

The Oman Mountains form probably the world's best exposed deformed continental margin and, as such, the region is an ideal field laboratory for the study of fundamental processes including rifting, passive margin development and thrust tectonics. The contributors discuss the sedimentary and structural evolution of the Mesozoic continental margin which is particularly relevant to oil and gas exploration in Oman.

The Oman Mountains form probably the world's best exposed deformed continental margin and, as such, the region is an ideal field laboratory for the study of fundamental processes including rifting, passive margin development and thrust tectonics. The contributors discuss the sedimentary and structural evolution of the Mesozoic continental margin which is particularly relevant to oil and gas exploration in Oman.

Much of the world's surface, even under the oceans, is covered in thick deposits of sedimentary particles - gravel, sand, silt and clay. The nature of the deposits and their formation is very much dependent on the distribution of particles of different sizes. However, different instruments measure different attributes of a particle's size, based on how fast a particle settles in water, or the surface area of a particle, or its length. This book provides information on the how and why of particle size analysis in terms of understanding these sediment deposits.

Much of the world's surface, even under the oceans, is covered in thick deposits of sedimentary particles - gravel, sand, silt and clay. The nature of the deposits and their formation is very much dependent on the distribution of particles of different sizes. However, different instruments measure different attributes of a particle's size, based on how fast a particle settles in water, or the surface area of a particle, or its length. This book provides information on the how and why of particle size analysis in terms of understanding these sediment deposits.