Alkali basalt

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Alkali basalt is one of the rocks comprising the Pali-Aike volcanic field, in Argentina.[1]

Alkali basalt or alkali olivine basalt is a dark-colored,

groundmass and phenocrysts, and nepheline in its CIPW norm.[4][5]

Geochemical characterization

Depiction of the total alkali-silica diagram. Alkali basalts are generally located in the upper left corner of the basalt region (region B).[6]

Alkali basalt is chemically classified as a rock in region B (basalt) of the total alkali versus silica (TAS) diagram that contains nepheline in its CIPW norm. Basalts that do not contain normative nepheline are characterized as sub-alkali basalts, which include tholeiitic basalts and calc-alkaline basalts.[6]

Petrography

The groundmass of alkali basalt is mainly composed of olivine, titanium-rich augite and

alkali feldspar or feldspathoid interstitially, but is poor in silica minerals, such as hypersthene and quartz.[4]

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 and iron oxides with lower frequency.[3][4]

Geologic context

Alkali basalt can be found in areas associated with volcanic activity, such as oceanic islands (Hawaii, Madeira,[7] Saint Helena,[8] Ascension, etc.), continental rifts and volcanic fields.[3] Continental alkali basalt can be found in every continent, with prominent examples being the Rio Grande Rift (USA), the East African Rift and the Pali-Aike volcanic field.[9]

The results from the

gamma ray spectrometer on Venera 8 on Venus suggest it landed on alkali basalt.[10]

References

External links