K-Ar data for the age and evolution of Gettysburg Bank, North Atlantic Ocean

Details K-Ar data for the age and evolution of Gettysburg Bank, North Atlantic Ocean K-Ar data for the age and evolution of Gettysburg Bank, North Atlantic Ocean

Aug 1979

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979e%26psl..44..261p&link_type=abstract

Earth and Planetary Science Letters, Volume 44, Issue 2, p. 261-268.

Computer Science

8

Scientific paper

Gettysburg Bank forms the western end of the Gorringe Seamount which is situated in the North Atlantic 110 km west of the tip of the Iberian Peninsula, on the eastern end of the Azores/Gibraltar fracture zone. Gabbros dredged from the Gettysburg Bank record a complex history of events. K-Ar ages of separated mineral phases fall into three concordant groups (plus some discordant ages). The oldest ages are from three brown kaersutitic hornblendes and their mean age of 135 +/- 3 Ma is taken to be that of their formation. Six plagioclase feldspars yielded concordant ages of 105 +/- 3 Ma which is possibly a consequence of a thermal event occurring at that time. Ages from three deformed plagioclases are concordant with a mean of 82 +/- 3 Ma which is believed to relate to a phase of shearing, perhaps occurring during transform motion at the plate boundary.

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