Phenocrysts are ubiquitous in alkali basalt and, similarly to the groundmass, are usually made up of olivine and titanium-rich augite but can also have plagioclase andiron oxides with lower frequency.[3][4]
^Skewes, Milka Alexandra; Stern, Charles R. (1979). "Petrology and geochemistry of alkali basalts and ultramafic inclusions from the palei-aike volcanic field in Southern Chile and the origin of the patagonian plateau lavas".Journal of Volcanology and Geothermal Research.6 (1–2):3–25.Bibcode:1979JVGR....6....3S.doi:10.1016/0377-0273(79)90044-1.
^abcHaldar, S. K. (2017).Platinum-Nickel-Chromium Deposits. Elsevier. p. 45.ISBN9780128020418.
^abcWinter, John DuNann (2001).An Introduction to Igneous and Metamorphic Petrology. Upper Saddle River, New Jersey: Prentice Hall. pp. 148, 182.ISBN0132403420.
^Irvine, T. N.; Baragar, W. R. A. (1971). "A Guide to the Chemical Classification of the Common Volcanic Rocks".Canadian Journal of Earth Sciences.8 (5):523–548.Bibcode:1971CaJES...8..523I.doi:10.1139/e71-055.
^Farmer, G.L. (2005). Rudnick, R.L. (ed.).Treatise on Geochemistry: The crust. Gulf Professional Publishing. p. 97.ISBN9780080448473.
^Ulivi, Paolo; Harland, David M (2007).Robotic Exploration of the Solar System Part I: The Golden Age 1957-1982. Springer. pp. 159–160.ISBN9780387493268.