Influence of Seismic Source Parameters on the Excitation Wavelet in Seismic Explorations Based on Numerical Simulation

<table class="table-group" id="tab2"><tr><td><table class="table"><tr><td class="thead-hr" colspan="5"><hr/></td></tr><tr class="thead"><td class="align_left"><i>ρ</i> (g·cm<sup>−3</sup>)</td><td class="align_center"><i>E</i> (GPa)</td><td class="align_center"><i>μ</i></td><td class="align_center"><i>θ</i></td><td class="align_center"><i>V</i><sub><i>p</i></sub> (m·s<sup>−1</sup>)</td></tr><tr><td class="thead-hr" colspan="5"><hr/></td></tr><tr><td class="align_left">2.694</td><td class="align_center">8.51</td><td class="align_center">0.363</td><td class="align_center">0.0022</td><td class="align_center">3218</td></tr><tr class="table-tr"><td colspan="5"><hr class="tbody-hr"/></td></tr></table></td></tr><tr class="table-fn"><td><div><i>ρ</i>, density; <i>E</i>, elastic modulus; <i>μ</i>, Poisson’s ratio of the rock; <i>θ</i>, failure strain; <i>V</i><sub><i>p</i></sub>, velocity of the longitudinal waves of the rock.<br/></div></td></tr></table>

<div>Parameters of the marine carbonate model.</div>

Advances in Civil Engineering

tab2

Table 2

Table 2: Influence of Seismic Source Parameters on the Excitation Wavelet in Seismic Explorations Based on Numerical Simulation 