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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Cross-references
British Tertiary Volcanic Province; Calc-alkaline rocks; Feldspathoidal rocks—genesis; Flood basalt; Igneous rocks—tectonic setting; Island arcs—petrology; Lunar petrology; Mafic and ultramafic inclusions in igneous rocks; Magmatic differentiation; Mid-ocean ridge and ocean-floor petrology; Ocean-island igneous rocks; Petrochemical calculations; Rift valley volcanism; Upper mantle—experimental petrology.
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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
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