Solution Exercise 4‌

The minimum principal stress (σ3) has to be the same value as T (tensile strength of the rock) in order for extension fractures be formed. Consequently, joints are formed in the limestone when the value of σ3 is equal to −27.5 MPa, the tensile strength T of the limestone. By the same token, the value of σ3 for the sandstone should be −6.25 MPa.

The green and red Mohr circles drawn in the Mohr diagrams below represent possible stress conditions under which extension fractures are generated in the limestone and sandstone, respectively.

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Structural Geology Applied to Fractured Aquifer Characterization Copyright © by Amélia João Fernandes, Alain Rouleau, Eurípedes do Amaral Vargas Junior. All Rights Reserved.