Oxygen isotope disequilibrium between quartz and sanidine from the Bandelier Tuff, New Mexico, consistent with a short residence time of phenocrysts in rhyolitic magma

Author:

Wolff John A,Balsley Steven D,Gregory Robert T

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference76 articles.

1. Tectonics of the Jemez lineament in the Jemez Mountains and Rio Grande rift;Aldrich;J. Geophys. Res.,1986

2. Direct evidence for the origin of low-18O silicic magmas: quenched samples of a magma chamber’s partially-fused granitoid walls, Crater Lake, Oregon;Bacon;Earth Planet. Sci. Lett.,1989

3. Bailey, R.A., Smith, R.L., Ross, C.S., 1969. Stratigraphic nomenclature of volcanic rocks in the Jemez Mountains, New Mexico. US Geol. Surv. Bull. 1274-P, pp. 1–19.

4. Baldridge, W.S., 1979. Petrology and petrogenesis of Plio-Pleistocene basaltic rocks from the central Rio Grande Rift, New Mexico, and their relation to rift structure. In: Riecker, R.E. (Ed.), Rio Grande Rift: Tectonics and Magmatism. American Geophysical Union, Washington, DC, pp. 323–353.

5. Balsley, S.D., 1988. The Petrology and Geochemistry of the Tshirege Member of the Bandelier Tuff, Jemez Mountains Volcanic Field, New Mexico, USA. M.Sc. thesis, University of Texas, Arlington, TX.

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