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Phenocryst (English Wikipedia)

Analysis of information sources in references of the Wikipedia article "Phenocryst" in English language version.

refsWebsite
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4doi.org
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4books.google.com
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2harvard.edu
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1worldcat.org
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1semanticscholar.org
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1fsu.edu
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1oxfordreference.com
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books.google.com

  • Smith, George I. (1964). Geology and Volcanic Petrology of the Lava Mountains, San Bernardino County, California. United States Geological Survey professional paper 457. Washington, D.C.: United States Geological Survey. p. 39. OCLC 3598916.
  • Gill, Robin (2011). Igneous Rocks and Processes: A Practical Guide. Hoboken, New Jersey: Wiley. p. 34. ISBN 978-1-4443-3065-6.
  • Some use a 1% boundary condition, Sen, Bibhas; Sabale, A. B. & Sukumaran, P. V. (2012). "Lava channel of Khedrai Dam, northeast of Nasik in western Deccan Volcanic province: Detailed morphology and evidences of channel reactivation". Journal of the Geological Society of India. 80 (3): 314–328. doi:10.1007/s12594-012-0150-8. S2CID 128608511. and Ocean Drilling Program, Texas A & M University (1991). Proceedings of the Ocean Drilling Program. Part A, Initial report. Vol. 140. National Science Foundation (U.S.). p. 52., while others suggest a limit of 5%. Piccirillo, E. M. & Melford, A. J. (1988). The Mesozoic Flood Volcanism of the Paraná Basin: Petrogenetic and Geophysical Aspects. São Paulo, Brazil: Universidade de São Paulo, Instituto Astronômico e Geofísico. p. 49. ISBN 978-85-85047-04-7. and Moulton, B. J. A.; et al. (2008). Volcanology of the Felsic Volcanic Rocks of the Kidd-Munro assemblage in Prosser and Muro Townships and Premininary Correlations with the Kidd Creek Deposit, Abitibi Greenstone Belt, Ontario. Geological Survey of Canada, Current Research, No. 2008-18. Ottawa: Geological Survey of Canada. p. 19. ISBN 978-1-100-10649-6.
  • Gill, Robin (2011). Igneous Rocks and Processes: A Practical Guide. Hoboken, New Jersey: Wiley. p. 21. ISBN 978-1-4443-3065-6.

doi.org

  • The minimum size boundary is arbitrary and not precise. It is based upon observation and may vary depending upon whether technical aids, such as a hand lens or a microscope are used or not. One analyst used a 100 μm limit on the size of crystals as that was the minimum that could be point-counted accurately by optical means. Murphy, M. D.; Sparks, R. S. J.; Barclay, J.; Carroll, M. R. & Brewer, T. S. (2000). "Remobilization of andesite magma by intrusion of mafic magma at the Soufriere Hills Volcano, Montserrat, West Indies". Journal of Petrology. 41 (1): 21–42. doi:10.1093/petrology/41.1.21.
  • Some use a 1% boundary condition, Sen, Bibhas; Sabale, A. B. & Sukumaran, P. V. (2012). "Lava channel of Khedrai Dam, northeast of Nasik in western Deccan Volcanic province: Detailed morphology and evidences of channel reactivation". Journal of the Geological Society of India. 80 (3): 314–328. doi:10.1007/s12594-012-0150-8. S2CID 128608511. and Ocean Drilling Program, Texas A & M University (1991). Proceedings of the Ocean Drilling Program. Part A, Initial report. Vol. 140. National Science Foundation (U.S.). p. 52., while others suggest a limit of 5%. Piccirillo, E. M. & Melford, A. J. (1988). The Mesozoic Flood Volcanism of the Paraná Basin: Petrogenetic and Geophysical Aspects. São Paulo, Brazil: Universidade de São Paulo, Instituto Astronômico e Geofísico. p. 49. ISBN 978-85-85047-04-7. and Moulton, B. J. A.; et al. (2008). Volcanology of the Felsic Volcanic Rocks of the Kidd-Munro assemblage in Prosser and Muro Townships and Premininary Correlations with the Kidd Creek Deposit, Abitibi Greenstone Belt, Ontario. Geological Survey of Canada, Current Research, No. 2008-18. Ottawa: Geological Survey of Canada. p. 19. ISBN 978-1-100-10649-6.
  • Byerly, Gary R. & Wright, Thomas L. (1978). "Origin of major element chemical trends in DSDP Leg 37 basalts, Mid-Atlantic Ridge". Journal of Volcanology and Geothermal Research. 3 (3–4): 229–279. Bibcode:1978JVGR....3..229B. doi:10.1016/0377-0273(78)90038-0.
  • Cox, S. F. & Etheridge, M. A. (1983). "Crack-seal fibre growth mechanisms and their significance in the development of oriented layer silicate microstructures". Tectonophysics. 92 (1): 147–170. Bibcode:1983Tectp..92..147C. doi:10.1016/0040-1951(83)90088-4.

fsu.edu

magnet.fsu.edu

harvard.edu

ui.adsabs.harvard.edu

oxfordreference.com

semanticscholar.org

api.semanticscholar.org

  • Some use a 1% boundary condition, Sen, Bibhas; Sabale, A. B. & Sukumaran, P. V. (2012). "Lava channel of Khedrai Dam, northeast of Nasik in western Deccan Volcanic province: Detailed morphology and evidences of channel reactivation". Journal of the Geological Society of India. 80 (3): 314–328. doi:10.1007/s12594-012-0150-8. S2CID 128608511. and Ocean Drilling Program, Texas A & M University (1991). Proceedings of the Ocean Drilling Program. Part A, Initial report. Vol. 140. National Science Foundation (U.S.). p. 52., while others suggest a limit of 5%. Piccirillo, E. M. & Melford, A. J. (1988). The Mesozoic Flood Volcanism of the Paraná Basin: Petrogenetic and Geophysical Aspects. São Paulo, Brazil: Universidade de São Paulo, Instituto Astronômico e Geofísico. p. 49. ISBN 978-85-85047-04-7. and Moulton, B. J. A.; et al. (2008). Volcanology of the Felsic Volcanic Rocks of the Kidd-Munro assemblage in Prosser and Muro Townships and Premininary Correlations with the Kidd Creek Deposit, Abitibi Greenstone Belt, Ontario. Geological Survey of Canada, Current Research, No. 2008-18. Ottawa: Geological Survey of Canada. p. 19. ISBN 978-1-100-10649-6.

worldcat.org

search.worldcat.org

  • Smith, George I. (1964). Geology and Volcanic Petrology of the Lava Mountains, San Bernardino County, California. United States Geological Survey professional paper 457. Washington, D.C.: United States Geological Survey. p. 39. OCLC 3598916.