词条 | Kenyte |
释义 |
Kenyte has a glassy texture and may be composed of devitrified glass, which contains large phenocrysts of anorthoclase feldspar.[4] References1. ^Roger Walter Le Maître, Igneous Rocks: A Classification and Glossary of Terms: Recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Igneous Rocks, Cambridge University Press; 2nd ed., 2002, p. 96 {{ISBN|978-0-521-66215-4}} {{petrology-stub}}2. ^J. W. Gregory, The Geological History of Mount Kenya, The Quarterly journal of the Geological Society of London, Volume 56, 1900, pp. 219-220 3. ^Kyle, Philip R., ed., Volcanological and Environmental Studies of Mount Erebus, Antarctica, American Geophysical Union (December 1994), p. xi {{ISBN|978-0-87590-875-5}} 4. ^{{cite web|title=Mt. Kenya Volcano |url=http://www1.newark.ohio-state.edu/Professional/OSU/Faculty/jstjohn/Volcano%20stuff/Mt.-Kenya.htm |accessdate=13 July 2011 |deadurl=yes |archiveurl=https://web.archive.org/web/20120326120008/http://www1.newark.ohio-state.edu/Professional/OSU/Faculty/jstjohn/Volcano%20stuff/Mt.-Kenya.htm |archivedate=26 March 2012 |df= }} 5 : Volcanic rocks|Igneous petrology|Mount Kenya|Geology of Kenya|Volcanism of Antarctica |
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