Vogel, Thomas A., Ryerson, Frederick J., Noble, Donald C., Younker, Leland W. (1987) Limits to Magma Mixing Based on Chemistry and Mineralogy of Pumice Fragments Erupted from a Chemically Zoned Magma Body. The Journal of Geology, 95 (5) 659-670 doi:10.1086/629162
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Limits to Magma Mixing Based on Chemistry and Mineralogy of Pumice Fragments Erupted from a Chemically Zoned Magma Body | ||
Journal | The Journal of Geology | ||
Authors | Vogel, Thomas A. | Author | |
Ryerson, Frederick J. | Author | ||
Noble, Donald C. | Author | ||
Younker, Leland W. | Author | ||
Year | 1987 (September) | Volume | 95 |
Page(s) | 659-670 | Issue | 5 |
Publisher | University of Chicago Press | ||
DOI | doi:10.1086/629162Search in ResearchGate | ||
Mindat Ref. ID | 165261 | Long-form Identifier | mindat:1:5:165261:5 |
GUID | 98737ec1-04a4-46ea-a2bc-16c4769e45f9 | ||
Full Reference | Vogel, Thomas A., Ryerson, Frederick J., Noble, Donald C., Younker, Leland W. (1987) Limits to Magma Mixing Based on Chemistry and Mineralogy of Pumice Fragments Erupted from a Chemically Zoned Magma Body. The Journal of Geology, 95 (5) 659-670 doi:10.1086/629162 | ||
Plain Text | Vogel, Thomas A., Ryerson, Frederick J., Noble, Donald C., Younker, Leland W. (1987) Limits to Magma Mixing Based on Chemistry and Mineralogy of Pumice Fragments Erupted from a Chemically Zoned Magma Body. The Journal of Geology, 95 (5) 659-670 doi:10.1086/629162 | ||
In | (1987, September) The Journal of Geology Vol. 95 (5) University of Chicago Press |
References Listed
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Not Yet Imported: Geological Society of America Special Papers - book-chapter : 10.1130/SPE180-p5 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 25243 | |
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Not Yet Imported: Geological Society of America Special Papers - book-chapter : 10.1130/SPE180-p5 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 25243 | |
VOGEL T. A. () Chemicalevolutionat a high-levelmagmasystem: the Black Mountain Volcanic Center | |
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