The undrained change in pore fluid pressure that accompanies dike intrusion may be conveniently represented as a moving volumetric dislocation. The concept of a
The Qooshchi area lies to northwest of Orumieh Lake in western Azerbaijan, NW Iran. A basement metamorphic complex, consisting of Precambrian schists and gneiss
The presence of a single Otoceras species (O. boreale), morphologically very variable, at the base of the Nekuchan Formation in Verkhoyansk, we believe, is to b