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• W2113293404 startingPage "357" @default.
• W2113293404 abstract "During November-December 1988, an extensive geophysical data set was collected over the Josephine Seamount, which is located at the northeasterly end of the Madeira-Tore Rise in the eastern North Atlantic. The Josephine Seamount lies at the intersection of the Madeira-Tore Rise and Azores-Gibraltar Fracture Zone, the latter representing the Africa-Eurasia plate boundary in this part of the eastern North Atlantic. From this data set, a 275 km long explosive refraction line has been modelled together with wide-angle airgun profiles, seismic reflection and gravity data. The velocity-depth model shows that the crust either side of the Seamount is typically oceanic in character. However, beneath the Seamount there exists a region of anomalously high velocity and crustal thickening to a depth of about 17-18 km. Gravity modelling also suggests that the Josephine Seamount is compensated by a crustal root, and that the Josephine Seamount/Madeira-Tore Rise system is in local isostatic equilibrium. Calculations of the flexural rigidity and effective elastic thickness of the lithosphere in this region suggest that the Madeira-Tore Rise formed contemporaneously with the lithosphere on which it lies. This age of crustal loading is consistent with the proposal that the Madeira-Tore Rise is an aseismic ridge which formed at or near the Mid-Atlantic Ridge." @default.
• W2113293404 created "2016-06-24" @default.
• W2113293404 creator A5027930507 @default.
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• W2113293404 date "1991-08-01" @default.
• W2113293404 modified "2023-09-26" @default.
• W2113293404 title "Crustal structure of the Madeira-Tore Rise, eastern North Atlantic-results of a DOBS wide-angle and normal incidence seismic experiment in the Josephine Seamount region" @default.
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• W2113293404 doi "https://doi.org/10.1111/j.1365-246x.1991.tb03898.x" @default.
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