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Titlebook: Natural Language Processing for the Semantic Web; Diana Maynard,Kalina Bontcheva,Isabelle Augenstein Book 2017 Springer Nature Switzerland

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樓主: Garfield
11#
發(fā)表于 2025-3-23 11:29:52 | 只看該作者
Diana Maynard,Kalina Bontcheva,Isabelle Augensteinrease of potential environmental risks in the region. Although devastating earthquakes are almost unknown in the area and seismic hazard is not great, the seism978-94-009-7048-9978-94-009-7046-5Series ISSN 1389-2185
12#
發(fā)表于 2025-3-23 14:53:53 | 只看該作者
Diana Maynard,Kalina Bontcheva,Isabelle Augenstein
13#
發(fā)表于 2025-3-23 18:14:15 | 只看該作者
n the overriding plate and the activation of the intermediate-depth earthquakes of down-dip tension type. After the occurrence of a large interplate earthquake, the activity of the intermediate-depth earthquakes of down-dip compression type in the subducting slab is expected to increase and migrate
14#
發(fā)表于 2025-3-23 23:00:21 | 只看該作者
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發(fā)表于 2025-3-24 04:37:51 | 只看該作者
16#
發(fā)表于 2025-3-24 10:18:53 | 只看該作者
Diana Maynard,Kalina Bontcheva,Isabelle Augensteinea of roof collapse and the area of active longwall mining are located between two east-striking loose vertical fracture zones. The characteristics of the seismic event suggest that it might have been sudden shear failure resulting from accumulated strain energy in overlying strata behind an active
17#
發(fā)表于 2025-3-24 12:59:46 | 只看該作者
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發(fā)表于 2025-3-24 18:44:08 | 只看該作者
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發(fā)表于 2025-3-24 22:27:13 | 只看該作者
Diana Maynard,Kalina Bontcheva,Isabelle Augenstein 12. Epicentre coordinates 12 2. 13. Epicentral intensity 13 2. 14. Description of macro seismic effects, foreshocks, aftershocks 14 2. 2. Statistical tables 15 2. 3. Supplementary catalogues for the years prior to 1801 and after 1955 17 2. 4. Catalogue of Earthquakes 1801-1900, 10 ~ VII 19 2. 41. Earthquake 978-94-010-3080-9978-94-010-3078-6
20#
發(fā)表于 2025-3-25 02:35:12 | 只看該作者
all survey and provide seismologists with unified parameters. Moreover, a survey map gives a better possibility of studying the seismotectonic relations between units of different tectonic types. Uniform parameters can be simply applied later in regional and more detailed studies, i. e. also in comp
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