Compositional variation in normal MORB from 22o-25oN: Mid- Atlantic ridge and Kane Fracture Zone

W. B. Bryan, G. Thompson, J. N. Ludden

Research output: Contribution to journalArticlepeer-review

128 Citations (Scopus)


Basalts collected by dredging between 23oN and 25oN include samples from the active spreading ridges, median valley walls, and older walls of the Kane Fracture Zone transform fault at about 24oN. There is no evidence of present or past volcanic activity within the transform zone. Petrogenesis of the basalts, is deduced from both petrographic and geochemical evidence. It is shown that a basalt-type common to the area is a logical choice as a mantle-derived primary magma; it is close to the composition of average normal MORB. We outline a comprehensive hypothesis for melting, fractionation, and mixing which we believe may be adequate to explain compositional variation in these and other suites of 'normal MORB'. An important consequence of this model is that MORB presently at a given position on a low-pressure, multiply saturated cotectic may have reached that point by a variety of paths; some may be nearly direct mantle derivatives, while others may have experienced a complex history of polybaric and low-pressure fractionation and/or mixing.-Authors

Original languageEnglish
Pages (from-to)11815-11836
Number of pages22
JournalJournal of Geophysical Research: Solid Earth
Issue numberB12
Publication statusPublished - 10 Dec 1981

ASJC Scopus subject areas

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology


Dive into the research topics of 'Compositional variation in normal MORB from 22o-25oN: Mid- Atlantic ridge and Kane Fracture Zone'. Together they form a unique fingerprint.

Cite this