斑晶 (Chinese Wikipedia)
Analysis of information sources in references of the Wikipedia article "斑晶" in Chinese language version.
refsWebsite
Global rank
Chinese rank
3rd place
8th place
6th place
4th place
1st place
1st place
5th place
12th place
938th place
1,605th place
archive.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. Remobilization of andesite magma by intrusion of mafic magma at the Soufriere Hills Volcano, Montserrat, West Indies. Journal of Petrology. 2000, 41 (1): 21–42. doi:10.1093/petrology/41.1.21
. - Williams, Howel; Turner, Francis J.; Gilbert, Charles M. Petrography: An introduction to the study of rocks in thin sections. San Francisco: W. H. Freeman. 1954: 102–103. ISBN 978-0-7167-0206-1.
books.google.com
- Smith, George I. 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. 1964: 39. OCLC 3598916.
- Gill, Robin. Igneous Rocks and Processes: A Practical Guide. Hoboken, New Jersey: Wiley. 2011: 34. ISBN 978-1-4443-3065-6.
- Some use a 1% boundary condition, Sen, Bibhas; Sabale, A. B.; Sukumaran, P. V. 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. 2012, 80 (3): 314–328. doi:10.1007/s12594-012-0150-8. and Ocean Drilling Program, Texas A & M University. Proceedings of the Ocean Drilling Program. Part A, Initial report 140. National Science Foundation (U.S.). 1991: 52., while others suggest a limit of 5%. Piccirillo, E. M.; Melford, A. J. The Mesozoic Flood Volcanism of the Paraná Basin: Petrogenetic and Geophysical Aspects. São Paulo, Brazil: Universidade de São Paulo, Instituto Astronômico e Geofísico. 1988: 49. ISBN 978-85-85047-04-7. and Moulton, B. J. A.; et al. 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. 2008: 19. ISBN 978-1-100-10649-6.
- Gill, Robin. Igneous Rocks and Processes: A Practical Guide. Hoboken, New Jersey: Wiley. 2011: 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. Remobilization of andesite magma by intrusion of mafic magma at the Soufriere Hills Volcano, Montserrat, West Indies. Journal of Petrology. 2000, 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. 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. 2012, 80 (3): 314–328. doi:10.1007/s12594-012-0150-8. and Ocean Drilling Program, Texas A & M University. Proceedings of the Ocean Drilling Program. Part A, Initial report 140. National Science Foundation (U.S.). 1991: 52., while others suggest a limit of 5%. Piccirillo, E. M.; Melford, A. J. The Mesozoic Flood Volcanism of the Paraná Basin: Petrogenetic and Geophysical Aspects. São Paulo, Brazil: Universidade de São Paulo, Instituto Astronômico e Geofísico. 1988: 49. ISBN 978-85-85047-04-7. and Moulton, B. J. A.; et al. 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. 2008: 19. ISBN 978-1-100-10649-6.
- Byerly, Gary R.; Wright, Thomas L. Origin of major element chemical trends in DSDP Leg 37 basalts, Mid-Atlantic Ridge. Journal of Volcanology and Geothermal Research. 1978, 3 (3): 229–279. doi:10.1016/0377-0273(78)90038-0.
- Cox, S. F.; Etheridge, M. A. Crack-seal fibre growth mechanisms and their significance in the development of oriented layer silicate microstructures. Tectonophysics. 1983, 92 (1): 147–170. doi:10.1016/0040-1951(83)90088-4.
fsu.edu
magnet.fsu.edu
- Gangopadhyay, A. M. I. T. A. V. A.; Sen, Gautam; Keshav, Shantanu. Experimental Crystallization of Deccan Basalts at Low Pressure: Effect of Contamination on Phase Equilibrium (PDF). Indian Journal of Geology. 2003, 75 (1/4): 54 [2021-11-04]. （原始内容存档 (PDF)于2010-06-15）.
oxfordreference.com
- "Crystal zoning." Oxford Reference. Accessed 8 Aug. 2020. https://www.oxfordreference.com/view/10.1093/oi/authority.20110803095651756 （页面存档备份，存于互联网档案馆）.
web.archive.org
- Gangopadhyay, A. M. I. T. A. V. A.; Sen, Gautam; Keshav, Shantanu. Experimental Crystallization of Deccan Basalts at Low Pressure: Effect of Contamination on Phase Equilibrium (PDF). Indian Journal of Geology. 2003, 75 (1/4): 54 [2021-11-04]. （原始内容存档 (PDF)于2010-06-15）.
- "Crystal zoning." Oxford Reference. Accessed 8 Aug. 2020. https://www.oxfordreference.com/view/10.1093/oi/authority.20110803095651756 （页面存档备份，存于互联网档案馆）.
worldcat.org
- Smith, George I. 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. 1964: 39. OCLC 3598916.