The Upper Crustal Evolution of a Large Silicic Magma Body: Evidence from Crystal-scale Rb–Sr Isotopic Heterogeneities in the Fish Canyon Magmatic System, Colorado-Reference-Cited by-同舟云学术

The Upper Crustal Evolution of a Large Silicic Magma Body: Evidence from Crystal-scale Rb–Sr Isotopic Heterogeneities in the Fish Canyon Magmatic System, Colorado

Published:2007-08-20 Issue:10 Volume:48 Page:1875-1894
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

Charlier B. L. A.,Bachmann O.,Davidson J. P.,Dungan M. A.,Morgan D. J.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/48/10/1875/16667036/egm043.pdf

Reference65 articles.

1. Volcanology, petrology and geochronology of the Fish Canyon magmatic system,;Bachmann,2001

2. Rejuvenation of the Fish Canyon magma body: a window into the evolution of large-volume silicic magma systems;Bachmann;Geology,2003

3. On the origin of crystal-poor rhyolites: extracted from batholithic crystal mushes;Bachmann;Journal of Petrology,2004

4. Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies;Bachmann;Journal of Volcanology and Geothermal Research,2006

5. Temperature-induced Al-zoning in hornblendes of the Fish Canyon magma, Colorado;Bachmann;American Mineralogist,2002

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