Titlebook: Geophysics of the Canary Islands; Results of Spain‘s E Peter Clift,Juan Acosta Book 2005 Springer Science+Business Media B.V. 2005 Geophysi

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Morphological and structural analysis in the Anaga offshore massif, Canary Islands: fractures and dNE-SW dominant direction of faulting was obtained, consistent with the Tenerife Island structural trend seen in the Anaga Massif and Cordillera Dorsal. NW-SE and E-W are two other main trends seen in the area. Special interest is manifest in two long faults: ‘Santa Cruz Fault’ bounds the southern ed

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A magnetic anomaly study offshore the Canary Archipelago, the archipelago, which lies between Tenerife and Gran Canaria Island, seems to be located at an average depth of 4 km below sealevel. A spectral analysis was performed to estimate the depth extent of the deepest anomalies. It argues the presence of sub-crustal magnetic sources (underplating) in the

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Paleoearthquake evidence in Tenerife (Canary Islands) and possible seismotectonic sources,d sand formation indicates an age of 10,081 ± 933 years, the liquefaction features ranging from this age to 3490 ± 473 years BP. This paleoearthquake was of much greater magnitude than those known historically. Faults with neotectonic activity are significant features that should be borne in mind wh

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nerife island..A detailed description of the archipelago gravity field and magnetic field of the Canary Islands..All in all the wealth of new data and ideas presented in this collection of papers has rarely been equaled in an investigation of an oceanic island group..978-94-007-8902-9978-1-4020-4352-9

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,Häufig verwendete Formelzeichen,es within a narrow region, 2) dike injection and volcanism shifting laterally through time, 3) volcanoes building nearly one atop of another in the Canary Islands, superimposing the stress field of one structure on the other and thus yielding a more complex distribution of gravitational stresses, an

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Elektromagnetische Schwingungen und Wellen the archipelago, which lies between Tenerife and Gran Canaria Island, seems to be located at an average depth of 4 km below sealevel. A spectral analysis was performed to estimate the depth extent of the deepest anomalies. It argues the presence of sub-crustal magnetic sources (underplating) in the

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Spektroskopie und Spektralanalyse,d sand formation indicates an age of 10,081 ± 933 years, the liquefaction features ranging from this age to 3490 ± 473 years BP. This paleoearthquake was of much greater magnitude than those known historically. Faults with neotectonic activity are significant features that should be borne in mind wh

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