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Titlebook: Geodetic And Geophysical Effects Associated With Seismic And Volcanic Hazards; José Fernández Book 2004 Springer Basel AG 2004 Geochemics.

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发表于 2025-3-21 16:42:44 | 显示全部楼层 |阅读模式
书目名称Geodetic And Geophysical Effects Associated With Seismic And Volcanic Hazards
编辑José Fernández
视频video
概述Modeling and simulations.Theoretical studies
丛书名称Pageoph Topical Volumes
图书封面Titlebook: Geodetic And Geophysical Effects Associated With Seismic And Volcanic Hazards;  José Fernández Book 2004 Springer Basel AG 2004 Geochemics.
描述Although geodetic monitoring techniques have been widely used in areas of seismic or volcanic activity, the difficulty inherent to their discrete nature means that they must be deployed carefully to ensure the best possible detection or sensitivity of these points (see e. g. , BALDI and UNGUENDOLI, 1987; JOHNSON and WYATT, 1994; SEGALL and MATTHEWS, 1997; Yu et al. , 2000). In many cases, a more global monitoring method, is required yet at the same time one that offers the highest level of sensitivity which enables detection of the phenomenon. Interferometry radar (InSAR) techniques have been shown to play an important role in seismic and volcanic monitoring because they cover large areas (100 x 100 km) and can be easily systematized in monitoring (see e. g. , MASSONNET and FEIGL, 1998; BDRGMANN et al. , 2000; MASSONNET and SIGMUNDSON, 2000; HANSSEN, 2001). The limitations inherent to the GPS and InSAR techniques (mainly observations at discrete surface points in the case of GPS and existence of non-coherent areas and the fact that, at present, the three displacement components cannot be obtained in SAR interferometry) can be overcome by using them together or other techniques (e.
出版日期Book 2004
关键词Geochemics; Geodesy; Seismicity; Volcanic Activity; earthquake; geophysics; microseism; seismic; volcano
版次1
doihttps://doi.org/10.1007/978-3-0348-7897-5
isbn_softcover978-3-7643-7044-2
isbn_ebook978-3-0348-7897-5Series ISSN 2504-3625 Series E-ISSN 2504-3633
issn_series 2504-3625
copyrightSpringer Basel AG 2004
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Stress Changes Modelled for the Sequence of Strong Earthquakes in the South Iceland Seismic Zone Siceland and the Eastern Volcanic Zone on the island. It is a transform zone, where earthquakes are expected to occur on E-W-trending left-lateral shear faults, equivalent to conjugate, N-S-oriented right-lateral, rupture planes. In fact, earthquakes take place on en-échelon N-S-oriented faults, which
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Comparison of Integrated Geodetic Data Models and Satellite Radar Interferograms to Infer Magma Stoo the InSAR data acquired during the second part. The geodetic changes are very marked in the first half of the eruption and constrain a deflation source located at a few kilometers of depth (≃ 3 km b.s.l.), in agreement with other independent geophysical evidence. SAR data, available during the sec
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GPS Monitoring in the N-W Part of the Volcanic Island of Tenerife, Canaries, Spain: Strategy and Ree deformation was detected using InSAR. To avoid undesirable antenna positioning errors in the stations built using nails, we designed and used calibrated, fixed-length metal poles, allowing us to guarantee that the GPS antenna was stationed with a height repeatability of the order of 1 mm and of le
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Gravity Changes and Internal Processes: Some Results Obtained from Observations at Three Volcanoes,en under investigation; each of them related to a plate boundary: Mayon/Luzon/Philippines, Merapi/Java/Indonesia, and Galeras/Colombia. The observed gravity changes are smaller than previously expected but significant. For the three volcanoes under investigation, and within the observation period, m
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The Interpretation of Gravity Changes and Crustal Deformation in Active Volcanic Areas,terpret geodetic and gravity data in active volcanic areas. This approach appears at odds with the real geology of volcanic regions, since the crust is not a homogeneous medium and magma chambers are not spheres. In this paper, we evaluate several more realistic source models that take into account
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