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Basalt

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Petrology

Part of the book series: Encyclopedia of Earth Science ((EESS))

Definition and classification

Basalts are fine-grained, mafic, volcanic rocks containing 44–53 wt% SiO2. They consist essentially of calcic plagioclase (An50+) and abundant mafic minerals, mainly Ca-rich clinopyroxene. Other phases include Ca-poor clinopyroxene, orthopyroxene, quartz, or olivine, feldspathoids (nepheline, leucite, analcime), small proportions of alkali feldspar (≪10% total feldspar), Fe–Ti oxides, and apatite. Amphibole phenocrysts or poikilocrysts may be present, and biotite may be included in the groundmass.

Basalts occur as lava flows, pillows, dykes, and sills. Their textures may be porphyritic or aphyritic, crystalline or glassy, ophitic or subophitic. Their most extensive form is as lava flows and pillows, in which they constitute the bulk of the ocean floor, major lava plateaus on the continents, and significant parts of volcanic edifices in rift valleys, ocean islands, and island arcs. They are the most important eruptive rocks on the Earth and Moon, and...

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© 1989 Van Nostrand Reinhold

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Jélinek, E., Holub, F.V., Klápová, H., Souček, J. (1989). Basalt . In: Petrology. Encyclopedia of Earth Science. Springer, Boston, MA. https://doi.org/10.1007/0-387-30845-8_24

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  • DOI: https://doi.org/10.1007/0-387-30845-8_24

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-0-442-20623-9

  • Online ISBN: 978-0-387-30845-6

  • eBook Packages: Springer Book Archive

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