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Titlebook: Natural Language Processing and Information Systems; 10th International C Andrés Montoyo,Rafael Muńoz,Elisabeth Métais Conference proceedin

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樓主: Adentitious
21#
發(fā)表于 2025-3-25 06:06:30 | 只看該作者
22#
發(fā)表于 2025-3-25 09:50:43 | 只看該作者
23#
發(fā)表于 2025-3-25 12:29:02 | 只看該作者
24#
發(fā)表于 2025-3-25 17:55:18 | 只看該作者
25#
發(fā)表于 2025-3-26 00:00:36 | 只看該作者
Jingbo Zhu,Wenliang Chenm Sinn der Glau-bens. in verschiedenen Bewu?tseinsakten wie der Perzeption oder Imagination, auch nicht die Glaubens?nderung im Sinn der Glaubens. in Zweifel, Negation usw.,. sondern eine ganz besondere Art von .modifikation. Das hei?t, es handelt sich bei einer solchen Modifikation um die Entstehun
26#
發(fā)表于 2025-3-26 02:25:50 | 只看該作者
27#
發(fā)表于 2025-3-26 07:11:40 | 只看該作者
Sofia Stamou,Vlassis Krikos,Pavlos Kokosis,Alexandros Ntoulas,Dimitris Christodoulakisrength, deformability, and damping in seismic design;.Reinforces concepts with real‐world examples;.Stands as a ready reference for performance‐based/risk-based seismic design, providing guidance for achieving a cost-effective seismic design..978-3-030-57860-2978-3-030-57858-9
28#
發(fā)表于 2025-3-26 10:11:57 | 只看該作者
Yunqing Xia,Wei Liu,Louise Guthrierength, deformability, and damping in seismic design;.Reinforces concepts with real‐world examples;.Stands as a ready reference for performance‐based/risk-based seismic design, providing guidance for achieving a cost-effective seismic design..978-3-030-57860-2978-3-030-57858-9
29#
發(fā)表于 2025-3-26 12:42:14 | 只看該作者
Yanbin Gao,Gang Zhaoction with the present flow pattern of the upper mantle convection. Effects of other mineralogic constituents, such as orthopyroxene and clinopyroxene in the upper mantle, and higher pressure phases and/or constituents with different chemistry at greater depths have to be taken into account (Anderso
30#
發(fā)表于 2025-3-26 19:44:43 | 只看該作者
Günther Fliedl,Christian Kop,Heinrich C. Mayr,Martin H?lbling,Thomas Horn,Georg Weber,Christian Winkction with the present flow pattern of the upper mantle convection. Effects of other mineralogic constituents, such as orthopyroxene and clinopyroxene in the upper mantle, and higher pressure phases and/or constituents with different chemistry at greater depths have to be taken into account (Anderso
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