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Titlebook: Geodynamics of Azores-Tunisia; E. Buforn,J. Martín-Dávila,A. Udías Book 2004 Springer Basel AG 2004 Deformation.Geodesy.Seismology.Seismot

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書(shū)目名稱(chēng)Geodynamics of Azores-Tunisia
編輯E. Buforn,J. Martín-Dávila,A. Udías
視頻videohttp://file.papertrans.cn/384/383123/383123.mp4
概述New analysis of recent geological, seismological, geodetic and paleomagnetic observations of the region from the Azores Islands to Tunisia.New models for the complex geodynamics of the Azores-Tunisia
叢書(shū)名稱(chēng)Pageoph Topical Volumes
圖書(shū)封面Titlebook: Geodynamics of Azores-Tunisia;  E. Buforn,J. Martín-Dávila,A. Udías Book 2004 Springer Basel AG 2004 Deformation.Geodesy.Seismology.Seismot
描述The following four papers deal with the seismicity and seismotectonic of the region. Carrilho et al. present the first results of GEOALGAR, a project initiated in 2000 to monitor the seismic activity in the Algarve region (southern Portugal). In this paper results of the relocation of epicenters and determination of fault plane solutions are presented. The new epicentral locations show a more organized spatial distribution which could indicate a possible correlation with some known tectonic features. Fault plane solutions are predominantly of strike-slip motion consistent with a horizontal compression in the NW-SE to NNW-SSE direction. The paper by Yelles-Chaouche et al. presents a detailed study of the 22 December, 1999 earthquake at Ain Temouchent (northwest Algeria) of magnitude 5. 7. The earthquake caused serious damage in the town of Ain Teemouchent with 25 casualties and 25000 people left homeless. Intensity map, surface features and the focal mechanism, based on wave form analysis, are shown. The mechanism corresponds to reverse fault motion with planes striking NNE-SSW resulting from horizontal compression in the NW-SE direction. This corresponds to the general mechanism fo
出版日期Book 2004
關(guān)鍵詞Deformation; Geodesy; Seismology; Seismotectonics; fault; geophysics; subduction; transform fault
版次1
doihttps://doi.org/10.1007/978-3-0348-7899-9
isbn_softcover978-3-7643-7043-5
isbn_ebook978-3-0348-7899-9Series ISSN 2504-3625 Series E-ISSN 2504-3633
issn_series 2504-3625
copyrightSpringer Basel AG 2004
The information of publication is updating

書(shū)目名稱(chēng)Geodynamics of Azores-Tunisia影響因子(影響力)




書(shū)目名稱(chēng)Geodynamics of Azores-Tunisia影響因子(影響力)學(xué)科排名




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Book 2004initiated in 2000 to monitor the seismic activity in the Algarve region (southern Portugal). In this paper results of the relocation of epicenters and determination of fault plane solutions are presented. The new epicentral locations show a more organized spatial distribution which could indicate a
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W. Graf ?u Leiningen-Westerburgumation caused by tectonic extrusion and concomitant extensional tectonics The extrusional/extensional tectonic setting is controlled by the SW-NE trending break-off scar left in the lithosphere of the Alboran Sea and SE Spain after detachment of a lithospheric slab The extruded material represents
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https://doi.org/10.1007/978-3-642-91079-1ef has been built up since Tortonian times, and is related to the development of folds and faults that are overprinted on older deformations, and some of the faults may be considered as out-of-sequence. The combination of geophysical and geological data makes it possible to determine the main featur
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Erratum to: Materialmengenermittlung,iption of the project goals, as well as the first results concerning the analysis of the recent seismic digital data, from 1999 and 2000, are presented. After simultaneous inversion of the seismic data and the velocity model parameters, the relocation of the hypocenters was performed for two selecte
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