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Figure 8: Typical stress-strain curves for rock materials.
Typical values of thermal conductivities of rock materials are given in the Table.
Typical stress-strain (deformation) curves for rock materials are shown in Figure 8.
The deviatoric stress state becomes an important element of any failure criterion used for rock materials.
The bigger Nakamura spectral ratio is, the higher the stress in coal and rock materials is.
The waste rock materials were generally low potential sources of acid mine drainage.
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Other studies deal with the host rock material.
Often a toe structure consists of rock material.
They occur when magma (molten rock material) congeals so rapidly that crystallization remains incomplete.
Folds and small faults may form at the foot of the slope where the rock material is under stress.
The main rock material of Puglia is limestone, except on the coastline, which is mostly low and sandy.
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