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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https://doi.org/10.1007/978-3-663-19201-5odesy and Oceanography) project in 1988. The measurements carried out between 1993 and 2000 (five campaigns) on nine GPS sites (one per island) were reprocessed using two state—of—the-art software packages. Different methodologies were applied to compute each campaign solution and the derived veloci

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,Die Mathematiker an der ETH Zürich,ones of the Betic Cordillera (Subbetic and Prebetic Zones). Progressive thermal demagnetisation of samples from the Subbetic Zone reveals the presence of two stable magnetic components of the natural remanent magnetisation: 1) a secondary Neogene syn-folding component and 2) the original Jurassic ma

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https://doi.org/10.1007/978-3-0348-7899-9Deformation; Geodesy; Seismology; Seismotectonics; fault; geophysics; subduction; transform fault

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Geodynamics of Azores-Tunisia978-3-0348-7899-9Series ISSN 2504-3625 Series E-ISSN 2504-3633

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