Peridotite xenoliths (green) in phonotephrite from Peridot Mesa , Arizona
Phonotephrite or phono-tephrite is a strongly alkaline volcanic rock with a composition between phonolite and tephrite .[ 1] This unusual igneous rock contains 7 to 12% alkali content and 45 to 53% silica content (see TAS diagram ). It can be described as a mafic phonolite or a potassic tephrite. Phonotephrite lava flows and volcanic cones have been identified in Antarctica (e.g. Mount Erebus ), Europe (e.g. Mount Vesuvius ), North America (e.g. Satah Mountain volcanic field ) and Africa (e.g. Jbel Saghro ).[ 2] [ 3] [ 4] [ 5]
See also
References
^ "Unusual Lava Types" . Strongly Alkaline Lavas . San Diego State University . Archived from the original on 2020-11-05. Retrieved 2016-09-11 .
^ P. Esser, Richard; R. Kyle, Philip; McIntosh, William C. (2004). "40 Ar/39 Ar dating of the eruptive history of Mount Erebus, Antarctica: volcano evolution". Bulletin of Volcanology . 66 (8). Springer : 671. Bibcode :2004BVol...66..671E . doi :10.1007/s00445-004-0354-x . S2CID 129118037 .
^ Kuehn, Christian; Guest, Bernard; K. Russell, James; A. Benowitz, Jeff (2015). "The Satah Mountain and Baldface Mountain volcanic fields: Pleistocene hot spot volcanism in the Anahim Volcanic Belt, west-central British Columbia, Canada". Bulletin of Volcanology . Springer : 8.
^ Berger, J.; Ennih, N.; Mercier, J.-C. C.; Liégeois, J.-P.; Demaiffe, D. (2009). "The role of fractional crystallization and late-stage peralkaline melt segregation in the mineralogical evolution of Cenozoic nephelinites/phonolites from Saghro (SE Morocco)". Mineralogical Magazine . 73 (1). Mineralogical Society of Great Britain and Ireland : 59. Bibcode :2009MinM...73...59B . doi :10.1180/minmag.2009.073.1.59 . ISSN 1471-8022 . S2CID 54866658 .
^ Pichavant, M.; Scaillet, B.; Pommier, A.; Iacono-Marziano, G.; Cioni, R. (2014). "Nature and Evolution of Primitive Vesuvius Magmas: an Experimental Study" . Journal of Petrology . 55 (11). Oxford University Press : 2281– 2310. doi :10.1093/petrology/egu057 .