Jan Mayen Microcontinent

Coordinates: 69°36′N 8°12′W / 69.6°N 8.2°W / 69.6; -8.2
Source: Wikipedia, the free encyclopedia.
Location of the Jan Mayen Microcontinent between the active Kolbeinsey Ridge, the inactive Aegir Ridge and the Jan Mayen Fracture zone

The Jan Mayen Microcontinent is a

Reykjanes Ridge separated this microcontinent from the Greenland Plate. For a short period it formed a microplate, until the Aegir Ridge became inactive, after which it formed part of the Eurasian Plate. The island of Jan Mayen is a much younger feature, formed of volcanic rock
, built up at the northernmost tip of the microcontinent.

Extent

The microcontinent extends about 500 km southwards from the Jan Mayen fracture zone. It is up to 160 km wide.[1] The Jan Mayen Ridge separates the Norwegian Sea (the Norway Basin) from the Greenland Sea.[2]

Identification

The microcontinent was identified originally on the basis of being a bathymetric high, a positive free-air gravity anomaly and due to the lack of magnetic anomalies, all indicating that it consisted of continental crust. This interpretation has been confirmed using wide-angle seismic reflection and refraction data,[3] coupled with standard normal incidence seismic reflection data.

Make-up

The microcontinent consists of the prominent bathymetric high, the Jan Mayen Ridge and several subsidiary ridges and intervening basins towards the south and west. Investigations using seismic reflection and refraction data have identified two passive margin sequences on the two sides of the microcontinent. Faults mapped on seismic reflection data are roughly N-S trending in the northern part becoming SW-NE trending to the south.[4] The crustal thickness reaches a maximum of 16 km on the eastern side of the main ridge.[5]

History

At the time of the initial break-up along the North Atlantic margin (Aegir Ridge in this area), the Jan Mayen Microcontinent formed part of the passive margin developed along the East Greenland margin.

Towards the end of the Eocene period, at about the time marked by

Late Eocene) a new spreading centre began to propagate northeastwards from the Reykjanes Ridge, forming the Kolbeinsey Ridge. During the period when both the Kolbeinsey and Aegir ridges were active, the microcontinent underwent a 30°–50° anti-clockwise rotation.[6][7][8] This was caused by the northeastward propagation of the Kolbeinsey Ridge, with simultaneous reduction in the rate of spreading at the southwestern end of the Aegir Ridge. An alternative but challenged model[6] involves no rotation but the development of several short-lived fracture zones cutting through the microcontinent.[4]
With both ridges active the microcontinent was also temporarily a microplate.

The Kolbeinsey Ridge reached the Jan Mayen Fracture Zone and therefore linked up to the

Late Oligocene to Early Miocene). At this time activity on the Aegir Ridge died away and the microcontinent became part of the Eurasian Plate. The northern end of the microcontinent was affected by renewed displacement on the Jan Mayen Fracture Zone. The volcanic island of Jan Mayen only formed in the Pleistocene,[5] possibly related to a hotspot, known as the Jan Mayen hotspot
, at the triple junction at the end of the Mohns Ridge.

Economic resources

The area around the microcontinent has recently become open for licensing for

Norwegian Petroleum Directorate.[10]

References

  1. Bibcode:2003AGUFM.T31D0872R
    .
  2. ^ C.Michael Hogan. 2011. Norwegian Sea. Eds. P.Saundry & C.J.Cleveland. Encyclopedia of Earth. National Council for Science and the Environment (U.S.) Washington DC
  3. doi:10.1046/j.1365-246X.1998.00444.x
    .
  4. ^
    ISBN 978-0-444-51849-1
    . Retrieved 2010-04-01.
  5. ^
    Bibcode:2003AGUFM.T12D0492B
    .
  6. ^
    doi:10.1016/j.marpetgeo.2012.02.015
    .
  7. doi:10.1016/S0264-8172(01)00046-0
    .
  8. Bibcode:2002AGUFM.T12D1344R
    .
  9. ^ The National Energy Authority (18 May 2009). "The First Licensing Round on the Icelandic continental shelf in the northern Dreki area is closed". Retrieved 2 July 2011.
  10. ^ Norwegian Petroleum Directorate (27 April 2011). "Seismic acquisition around Jan Mayen this summer". Retrieved 2 July 2011.

69°36′N 8°12′W / 69.6°N 8.2°W / 69.6; -8.2

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