Jelaskan Lihat juga dari Ignimbrit

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Branney M.J., Barry T.L., Godchaux M. (2004) Sheathfolds in rheomorphic ignimbrites. Bulletin of Volcanology. Vol 66, pp 485–491

Sparks R.S.J.(1976) Grain size variations in ignimbrites and implications for the transport of pyroclastic flows. Sedimentology 23, 147-188

Chapin C.E., Lowell G.R. (1979) Primary and secondary flow structures in ash-flow tuffs of the Gribbles Run paleovalley, central Colorado. Geology Society of America Special Paper. Vol 180, pp 137–154

Schmincke .H.-U, Swanson D.A. (1967) Laminar viscous flowage structures in ash-flow tuffs from Gran Canaria, Canary Islands. Geology. Vol 75, pp641–664

Freundt A. (1998) Formation of high grade ignimbrites Part II A pyroclastic suspension current model with implications for low grade ignimbrites. Bulletin of Volcanology. Vol 60, pp 545–567

Perez W., Alvarado G.E., GANS P.B (2006) The 322ka Tiribi Tuff: stratigraphy, geochronology and mechanisms of deposition of the largest and most recent ignimbrite in Valle Central, Costa Rica. Bulletin of Volcanology. Vol 69, pp 25–40

Ragan D.M., Sheridan M.F. (1972) Compaction of the Bishops Tuff. Geology society of America special bulletin. Vol 83, pp 95–106

Wolff J.A., Wright J.V. (1981) Rheomorphism of welded tuffs. Journal of Volcanology and Geothermal Research 10: 13–34

Kobberger G., Schmincke H. U. (1999) Deposition of rheomorphic ignimbrite D (Morgan Formation), Gran Canaria, Canary Islands, Spain. Bulletin of Volcanology. Vol 60, pp 465–485

Dictionary of New Zealand Biography, Patrick Marshall 1869-1950, http://www.dnzb.govt.nz/dnzb/default.asp?Find_Quick.asp?PersonEssay=3M44