Sentence examples for the subsidence process from inspiring English sources

The subsidence process is suppressed under the stamp grooves where neither alkali evacuation nor nanoparticle dissolution occurs.

From these facts, it is unlikely that the subsidence process relaxed naturally with a certain time constant after (1).

A proper form of influence function should be carefully defined so that it can well represent the mechanism involved in the subsidence process.

A new technology called CMR-UM (concurrent mining and reclamation for underground mining) was developed in China, which is done before or during the subsidence process.

Unfortunately, the interferograms of each of the three satellites were not directly comparable; however, the rate of subsidence in (2) was likely larger than the extension of the natural subsidence process (e.g., exponential decay) following period (1).

Two concepts have been devised with special regard to the mining subsidence process and seem to be adaptable especially to discontinuous materials.

In considering the development of the computer-based prediction methodology, it is important to predict 4D ground subsidence components at any point with any shape of excavation so as to cover a wide range of mining geometry as well as to provide automation, intellection, and visualization in the simulation of subsidence process.

A subsidence process then followed, with the shape of the deformation forming a mirror image of the uplift.

During most of its geological history, it was in a stable subsidence process except for a short period of traceable regional instability in the upper Cretaceous Turonian Stage (Murris 1980; Berberian and King 1981; Koop and Kholief 1982; Alsharhan and Nairn 1997; Alavi 2004).

Situations that change the local hydrogeology, such as dams, water abstraction, or injection/drainage, can accelerate dissolution and subsidence processes, increasing the severity of the problems; dams and canals built on gypsum karst can leak or fail catastrophically.

This work integrates detailed geological and hydrogeological information with PSI data to obtain a better understanding of subsidence processes detected in the detrital aquifer of the Vega de Granada (SE Spain) during the past 13 years.