norite

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Names in other languages

  • Englishnorite
  • Españolnorita
  • FrançaisNorite
  • Portuguêsnorito
  • עבריתנוריט
  • PolskiNoryt
  • РусскийНорит
  • УкраїнськаНорит

Article bodies are English and are not machine-translated. A name in another language is not a translation of the article.

valley on the moon during the Apollo 17 mission (sample 78236). Norite is a mafic intrusive igneous rock composed largely of the calcium-rich plagioclase labradorite, orthopyroxene, and olivine. The name norite is derived from Norway, by its Norwegian name Norge. Norite, also known as orthopyroxene gabbro, may be essentially indistinguishable from gabbro without thin section study under the petrographic microscope. The principal difference between norite and gabbro is the type of pyroxene of which it is composed. Norite is predominantly composed of orthopyroxenes, largely high-magnesian enstatite or an iron-bearing hypersthene. The principal pyroxenes in gabbro are clinopyroxenes, generally iron-rich augites. Norite occurs with gabbro and other mafic to ultramafic rocks in layered intrusions which are often associated with platinum orebodies such as in the Bushveld Igneous Complex in South Africa, the Skaergaard igneous complex of Greenland, and the Stillwater igneous complex in Montana. Norite is also the basal igneous rock of the Sudbury Basin complex in Ontario, which is the site of a comet impact and the world's second-largest nickel mining region. Norite is a common rock type of the Apollo samples. On a smaller scale, norite can be found in small localized intrusions such as the Gombak norite in Bukit Batok, Singapore.…

valley on the moon during the Apollo 17 mission (sample 78236). Norite is a mafic intrusive igneous rock composed largely of the calcium-rich plagioclase labradorite, orthopyroxene, and olivine. The name norite is derived from Norway, by its Norwegian name Norge. Norite, also known as orthopyroxene gabbro, may be essentially indistinguishable from gabbro without thin section study under the petrographic microscope. The principal difference between norite and gabbro is the type of pyroxene of which it is composed. Norite is predominantly composed of orthopyroxenes, largely high-magnesian enstatite or an iron-bearing hypersthene. The principal pyroxenes in gabbro are clinopyroxenes, generally iron-rich augites. Norite occurs with gabbro and other mafic to ultramafic rocks in layered intrusions which are often associated with platinum orebodies such as in the Bushveld Igneous Complex in South Africa, the Skaergaard igneous complex of Greenland, and the Stillwater igneous complex in Montana. Norite is also the basal igneous rock of the Sudbury Basin complex in Ontario, which is the site of a comet impact and the world's second-largest nickel mining region. Norite is a common rock type of the Apollo samples. On a smaller scale, norite can be found in small localized intrusions such as the Gombak norite in Bukit Batok, Singapore. It is also plentiful in the Sokndal intrusion area of southwestern Norway, with titanium deposits to the east.

References

Text derived from https://en.wikipedia.org/w/index.php?oldid=1374863404 under CC BY-SA 4.0; modifications have been made.

Provenance

snapshot norite-171258-3be70444675e28e6 · hash 3be70444675e28e6ec5e336d7e89658a34883178130ab5cd5582a9c471992d0c · captured 1789387222.0 · version history

Cite this page as: encyclopegia.org, “norite”, snapshot norite-171258-3be70444675e28e6. https://encyclopegia.org/a/norite

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