Kiruna porphyry

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Kiruna porphyry (Swedish : Kirunaporfyr) is a group of igneous rocks found near Kiruna in northernmost Sweden. [1] The Kiruna Porphyry formed 1,880 to 1,900 million years ago [1] [2] during the Paleoproterozoic Era in connection to the Svecofennian orogeny. [2]

The iron-apatite ore mined in Kiruna, Malmberget and Svappavaara are all hosted in Kiruna porphyry. [2] While generally well-preserved for its age at some locations such as Malmberget the Kiruna porphyry is more metamorphosed. [1]

In detail, various rock types are distinguished in the Kiruna porphyry such as trachyandesite lava and quartz-bearing porphyry of rhyolitic composition. [1] These two rocks are traditionally known as "syenite porphyry" and "quartz porphyry" respectively (Swedish : syenitporfyr , kvartsporfyr). [2] [1] The former is found on the foot wall of the Kiruna iron ore body, while the latter is found in the hanging wall. [1] Part of the quartz-bearing porphyry is thought to be ignimbrite. [1] The Haparanda Series of rocks found to east near the Sweden-Finland border are thought to have the same origin as the Kiruna porphyry. [3]

See also

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References

  1. 1 2 3 4 5 6 7 Lundqvist, Thomas (2009). Porfyr i Sverige: En geologisk översikt (in Swedish). pp. 24–25. ISBN   978-91-7158-960-6.
  2. 1 2 3 4 "kirunaporfyrer". Nationalencyklopedin (in Swedish). Retrieved 12 December 2019.
  3. Brewer, T.S.; Pharao, T.C. (1990). "Early Precambrian basic rocks of the Baltic Shield". In Hall, R.P.; Hughes, D.J. (eds.). Early Precambrian Basic Magmatism. Blackie. p. 291.