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Titlebook: Universities in Arab Countries: An Urgent Need for Change; Underpinning the Tra Adnan Badran (Editor-in-Chief),Elias Baydoun,John Book 201

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31#
發(fā)表于 2025-3-26 22:17:30 | 只看該作者
32#
發(fā)表于 2025-3-27 01:58:12 | 只看該作者
Milad Sebaalying the . values for corresponding models with (anelastic) and without (elastic) absorption. For the models considered in this study, the values of coda .. in anelastic media are in good agreement with the sum of the corresponding scattering .. and intrinsic .. values, as established by the single-s
33#
發(fā)表于 2025-3-27 07:23:16 | 只看該作者
Nidhal Guessoumserved wave field (so-called true amplitude concept) and thus require the proposed separation. The separation also has an important impact on computer time savings in modeling seismic wave fields generated by point sources by the ray method. For a given position in a given model, it is sufficient to
34#
發(fā)表于 2025-3-27 10:06:44 | 只看該作者
35#
發(fā)表于 2025-3-27 14:52:29 | 只看該作者
Nuhad J. Daghirf permeability, high complexity is observed in the spatio-temporal variation of rupture activity. For example, frequency-magnitude statistics of intermediate-size events are shown to obey the Gutenberg–Richter relation. Rupture sequences with features of earthquake swarms can be simulated when the r
36#
發(fā)表于 2025-3-27 19:58:44 | 只看該作者
37#
發(fā)表于 2025-3-27 22:07:11 | 只看該作者
38#
發(fā)表于 2025-3-28 03:36:19 | 只看該作者
Kamal F. Badrboreholes was drilled in the Andreevskii seam, but several bursts occurred during this period: seven were recorded during rise borehole drilling, one during horizontal borehole drilling, and three during mining operations in the face. Most of the bursts were small save the last one, Tolstyi seams. S
39#
發(fā)表于 2025-3-28 07:36:58 | 只看該作者
40#
發(fā)表于 2025-3-28 11:00:08 | 只看該作者
nic signal within this scatter. In the Sanriku (Japan) and Mexico subduction zones, underthrusting earthquakes that occur at the up-dip and down-dip edges of the seismogenic zone have correspondingly low and high values of stress drop. A speculative picture of the stress state of subduction zones em
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