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tectonic forces
The corresponding samples were taken in nontransform zones where rocks have experienced the action of significant tectonic forces and, moreover, anomalous geomagnetic field patterns correlate with the position of these zones.
      
Some phenomena such as the arc-shape mountain systems, volcanism and crustal deformation imply that the juncture zone of eastern and western tectonic forces is located at about 110°E.
      
Tectonic forces from the relative movements between plates are transmitted into the continental crust, and then they create the earthquake generating stress field there.
      
Fractures or interlayer-gliding are very likely to occur under the action of tectonic forces and thus to induce earthquakes in these areas.
      
The deviatoric stress estimates are further superposed on inferred stresses due to the regional plate tectonic forces.
      
The author of the paper discusses the influence of tectonic forces on coal which is clearly shown by the structure of deformed coal seams.
      
These collapse craters were evidently caused by the late-tectonic forces due to the northern Tharsis and adjoining lava loads, resulting in flexural tension and activating previous faults.
      
The state of stress around a noncircular working under the action of tectonic forces
      
Stressed state of rock surrounding excavations under mountainous relief and subject to tectonic forces
      
The boundary-element method is used for studying the stress state of rocks in the vicinity of the extensive cavity with gas depending on the actual gravitational and tectonic forces, gas pressure, as well as deposit geometry.
      
This model contains two essential elements: (i) Intersecting faults near Koyna provide means of stress build-up in response to plate tectonic forces.
      
If the lithospheric plate is acted upon by distant tectonic forces, strain accumulation must occur in a broad region.
      
One node (denoted by A) is loaded by external tectonic forces at a constant rate, with `events' (main shocks) occurring at random instances with risk given by a function of the `stress level' at the node.
      
A fracture in the subsurface rock caused by tectonic forces is called a fault.
      
Genesis of such equilibrium is equality of tectonic forces and friction forces of rock formation.
      
It is foundering, being extended in a NE-SW direction by regional tectonic forces.
      
It is a graben valley separated by horst mountain blocks as a result of extensional tectonic forces.
      
Loading mimics the impact of tectonic forces, and failures simulate earthquakes.
      
Loading in the model imitates the influence of tectonic forces, while failures imitate earthquakes.
      
Most movement occurs along narrow zones between plates where the results of plate-tectonic forces are most evident.
      
 

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