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John C. Eichelberger
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Journal Article

Calcic cores of plagioclase phenocrysts in andesite from Karymsky volcano: Evidence for rapid introduction by basaltic replenishment

Pavel E. Izbekov, John C. Eichelberger, Lina C. Patino, Thomas A. Vogel, Boris V. Ivanov
Journal: Geology
Published: 01 September 2002
Geology (2002) 30 (9): 799–802.
DOI: https://doi.org/10.1130/0091-7613(2002)030<0799:CCOPPI>2.0.CO;2
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Reply

John C. Eichelberger, Darren G. Chertkoff, Scott T. Dreher, Christopher J. Nye
Journal: Geology
Published: 01 November 2001
Geology (2001) 29 (11): 1063–1064.
DOI: https://doi.org/10.1130/0091-7613(2001)029<1064:>2.0.CO;2
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Magmas in collision: Rethinking chemical zonation in silicic magmas

John C. Eichelberger, Darren G. Chertkoff, Scott T. Dreher, Christopher J. Nye
Journal: Geology
Published: 01 July 2000
Geology (2000) 28 (7): 603–606.
DOI: https://doi.org/10.1130/0091-7613(2000)28<603:MICRCZ>2.0.CO;2
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New structural limits on magma chamber locations at the Valley of Ten Thousand Smokes, Katmai National Park, Alaska

Peter C. Wallmann, David D. Pollard, Wes Hildreth, John C. Eichelberger
Journal: Geology
Published: 01 December 1990
Geology (1990) 18 (12): 1240–1243.
DOI: https://doi.org/10.1130/0091-7613(1990)018<1240:NSLOMC>2.3.CO;2
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Origin of andesite and dacite: Evidence of mixing at Glass Mountain in California and at other circum-Pacific volcanoes

JOHN C. EICHELBERGER
Journal: GSA Bulletin
Published: 01 October 1975
GSA Bulletin (1975) 86 (10): 1381–1391.
DOI: https://doi.org/10.1130/0016-7606(1975)86<1381:OOAADE>2.0.CO;2
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Magma contamination within the volcanic pile: Origin of andesite and dacite: Comment and Reply: REPLY …

John C. Eichelberger
Journal: Geology
Published: 01 April 1975
Geology (1975) 3 (4): 164–168.
DOI: https://doi.org/10.1130/0091-7613(1975)3<164b:MCWTVP>2.0.CO;2
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Magma Contamination within the Volcanic Pile: Origin of Andesite and Dacite

John C. Eichelberger
Journal: Geology
Published: 01 January 1974
Geology (1974) 2 (1): 29–33.
DOI: https://doi.org/10.1130/0091-7613(1974)2<29:MCWTVP>2.0.CO;2
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