响岩質碱玄岩

响岩質碱玄岩（）是一種強鹼性火山岩，其成分介於响岩和碱玄岩之間 P. Esser, Richard; R. Kyle, Philip; McIntosh, William C. (2004). "40Ar/39Ar dating of the eruptive history of Mount Erebus, Antarctica: volcano evolution". Bulletin of Volcanology. Springer. 66 (8): 671. Bibcode:2004BVol...66..671E. doi:10.1007/s00445-004-0354-x. S2CID 129118037. 。 該火成岩含鹼量為 7% 至 12% 的和含二氧化矽量為45% 至 53% 的（參見 TAS 圖）。 它亦可稱為鎂鐵質響岩或鉀質碱玄岩。含响岩質碱玄岩的熔岩流和火山錐目前已出露在南極洲（例如埃里伯斯山）、歐洲（例如維蘇威火山）、北美（例如薩塔山火山場）和非洲（例如 Jbel Saghro）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. Mineralogical Society of Great Britain and Ireland. 73 (1): 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. Oxford University Press. 55 (11): 2281–2310. doi:10.1093/petrology/egu057.。
參考文獻

Category:基性岩
Category:火山岩