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Doklady Earth Sciences

, Volume 437, Issue 1, pp 343–348 | Cite as

Tectonic evolution of the Knipovich Ridge based on the anomalous magnetic field

  • S. Yu. Sokolov
Geology

Abstract

Calculation of the downward continuation for the anomalous magnetic field at the Knipovich Ridge showed more complicate segmentation of the spreading oceanic basement than was earlier considered. The structural pattern of the field is evidence that the area consists of no less than four segments separated by transform fracture zones with the azimuth of oceanic crust accretion about 310° and the normal position relative to the rift segments with the azimuth of 40°. The modern location of the axis of the Knipovich Ridge straightens the complicate divergent boundary between the plates in the strike-slip conditions between the spreading centers of the Mohns and Gakkel ridges. The axis is a detachment zone intersecting the oceanic basement having formed from the Late Oligocene. A new magnetoactive layer composed of magmatic products has not yet been formed in this structure.

Keywords

Strike Slip Downward Continuation Knipovich Ridge Detachment Zone Gakkel Ridge 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Pleiades Publishing, Ltd. 2011

Authors and Affiliations

  • S. Yu. Sokolov
    • 1
  1. 1.Geological InstituteRussian Academy of SciencesMoscowRussia

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