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In practice this concept is used as a proxy model for rough estimations of basic rock properties and for educational purposes


left

1
mathblock

LaTeX Math Inline

alignment
bodyh_e

({\bf

r})

=

{\rm

const}

2
mathblock

LaTeX Math Inline

alignmentleft

body\phi_e({\bf

r})

=

{\rm

const}

\

quad

\rightarrow

\ c_r({\bf

r})

=

{\rm

const}

3No fractures, no faults



See Also

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