The transitional pressure of quartz-coesite under the differential stress and highly-strained conditions is far from the pressure of the stable field under the
The formation process of the Dianqiangui basin, a special basin, occurred after the Caledonian orogeny, in the south of Guizhou, the west of Guangxi and the sou
The undrained change in pore fluid pressure that accompanies dike intrusion may be conveniently represented as a moving volumetric dislocation. The concept of a