Petrology and mineralogy of dredged gabbro from Gettysburg Bank, eastern Atlantic View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1982-04

AUTHORS

H. M. Prichard, J. R. Cann

ABSTRACT

Gabbros have been dredged from Gettysburg Bank, 110 km west of Portugal on the Azores/Gibraltar fracture zone. Primary minerals in olivine, pyroxene and brown hornblende gabbros are partially replaced by metamorphic minerals. Igneous textures are inhomogeneously overprinted by a granular polyhedral deformation and a cataclastic deformation. Amphiboles show characteristics which indicate a transition from crystallisation in a magma chamber to formation of amphibole in solid gabbro under metasomatic conditions. Of the amphiboles analysed, chlorine was present in the green amphiboles but below 0.05% in the brown suggesting the penetration of sea water after the formation of the brown amphibole but during the formation of the green. More... »

PAGES

46-55

References to SciGraph publications

  • 1978-06. Origin of chlorine and bromine in the oceans in NATURE
  • 1974. The Azores-Gibraltar Plate Boundary in GEODYNAMICS OF ICELAND AND THE NORTH ATLANTIC AREA
  • 1970-11. Nepheline Gabbro from the Mid-Atlantic Ridge in NATURE
  • 1978-03. Cl and Br degassing by volcanism along the Reykjanes Ridge and Iceland in NATURE
  • 1969-12. The metasomatic development of zoned ultrabasic bodies in Unst, Shetland in CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
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    http://scigraph.springernature.com/pub.10.1007/bf00376960

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    http://dx.doi.org/10.1007/bf00376960

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