Titlebook: Structure and Development of the Greenland-Scotland Ridge; New Methods and Conc Martin H. P. Bott,Svend Saxov,J?rn Thiede Book 1983 Springe

ANTH

Geology and Crustal Structure of the Faeroe Islands - A Reviewhe 200 m contour line the basalts are overlain by sediments reaching a thickness of 2 km. The shelf is separated from the Iceland-Faeroe Ridge by a scarp with a gravimetric anomaly, and the Faeroese crust has lower velocities (6.2 km/s or less) than the crust of the ridge (6.7 km/s). The Faeroese cr

Meander

Aspects of the Tertiary Geology of the Faeroe-Shetland Channelhis, the southeast flank of the Faeroe Basin, in particular the Tertiary stratigraphy and occurrences of igneous rocks..A Palaeocene hinge-line can be traced along the basin flank and it is accompanied by listric growth- faults. The Eocene-Oligocene hinge-line is northwest of the Palaeocene one and

accordance

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legacy

審問

稀釋前

外來

Ocean-Bottom Seismographsdata include recordings of controlled sources (explosions and airguns) and of earthquakes. Instruments which cannot be used in typically oceanic depths are not discussed. Reviews of some early OBS have been written by Ewing and Ewing and by Bradner.. In this paper the widely-used acronym OBS stands

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Outstanding Geological Problems of the Greenland-Scotland Ridge: An Introductionh have been discussed but not solved during the advanced study institute in Bressanone/Italy during May 1981. The diverse opinions of the individual authors on problems such as for example the nature of the basement under the Faeroe Islands, the origin and type of volcanism building the ridge, the a