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This obviates the need for acquiring and employing the mathematical knowledge involving principal and intermediate convergents computed using a polynomial-time algorithm for practical problems.
In the juvenile specimens, the principal and intermediate denticles are more uniform, being of similar length and morphology; however, in the adult specimens, there is strong differentiation between and within the principal and intermediate denticles.
The juvenile chelicerae clearly exhibit the Jaekelopterus denticulation pattern and show similar trends to those noted in juvenile chelicerae of Jaekelopterus rhenaniae by Poschmann and Tetlie [ 69]: specifically, a more gracile terminal denticle and less differentiation between the principal and intermediate denticles.
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The free ramus is consistent between the juvenile and adult morphologies in possessing a terminal denticle along with three principal and five intermediate denticles.
The stress strain behavior of Fine Nevada sand is presented for discrete combinations of constant principal stress direction, α, and intermediate principal stress.
Besides, when the minimum principal stress is large and the difference between minimum and intermediate principal stress is larger, brittle failure occurs along tensile-shear fractures.
Following the optimization of architecture and configuration of ANNs, the training data are used for training the networks to predict the value of major principal stress at failure from the values of minor and intermediate principal stresses.
True triaxial tests with different levels of minor and intermediate principal stress are simulated.
All in all, the degree of anisotropy has a great effect on the maximum and intermediate principal stresses.
Their inversion results yield maximum and intermediate principal stress axes close to horizontal and minimum compressive stress axis far from horizontal, suggesting a transpressive tectonic stress regime in the western part of the Gulf of Izmit.
The inversion results show that the maximum and intermediate principal stress axes are closer to horizontal and that the minimum compressive stress axis is closer to vertical, indicating a transpressive tectonic stress regime (Table 1) in the western part of the Gulf of Izmit, which well fits the structural models (Gökaşan et al., 2001; Cormier et al., 2006).
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