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Titlebook: Developments in Four-Dimensional Geodesy; Selected papers of t Fritz K. Brunner,Chris Rizos Conference proceedings 1990 Springer-Verlag Ber

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書(shū)目名稱Developments in Four-Dimensional Geodesy
副標(biāo)題Selected papers of t
編輯Fritz K. Brunner,Chris Rizos
視頻videohttp://file.papertrans.cn/271/270193/270193.mp4
叢書(shū)名稱Lecture Notes in Earth Sciences
圖書(shū)封面Titlebook: Developments in Four-Dimensional Geodesy; Selected papers of t Fritz K. Brunner,Chris Rizos Conference proceedings 1990 Springer-Verlag Ber
描述This selection of papers emphasizes the advances in the field and covers a wide range of topics in geophysics, geodynamics, and oceanography to which modern geodesy is contributing.
出版日期Conference proceedings 1990
關(guān)鍵詞Deformation; Ocean; Oceanography; Ozeanographie; Schwere; Tektonik; Vierdimensionale Geod?sie; geodesy; geop
版次1
doihttps://doi.org/10.1007/BFb0009877
isbn_softcover978-3-540-52332-1
isbn_ebook978-3-540-46961-2Series ISSN 0930-0317 Series E-ISSN 1613-2580
issn_series 0930-0317
copyrightSpringer-Verlag Berlin Heidelberg 1990
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Absolute gravimetry as an operational tool for geodynamics research,geodynamics research by monitoring vertical crustal movements and internal mass shifts. With today‘s accuracy of about ± 0.05μms. (or 5μGal), significant results have been obtained in numerous control nets of local extension, especially in connection with seismic and volcanic events. Nevertheless, t
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Satellite gravity gradiometry: A future technique for global high resolution gravity field recoveryracking, is satellite gravity gradiometry. In this paper the current state of the art of gravity field determination is sketched as well as the need for an improvement of our knowledge of the gravity field. Then the structure of the tidal field is discussed and the basic mechanical principles of sat
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Four dimensional adjustment of the finnish first-order triangulation: Results of a test computationl as the crustal deformations possibly taking place in the area for such a study; the area in question belongs geologically to the Fennoscandian Shield..The strain patterns found agree with those obtained from geological considerations. Because the time span between the triangulation and the trilate
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