Water–Rock interactions in the basement beneath Long Valley Caldera: an oxygen isotope study of the Long Valley Exploratory Well drill cores-Reference-Cited by-同舟云学术

Water–Rock interactions in the basement beneath Long Valley Caldera: an oxygen isotope study of the Long Valley Exploratory Well drill cores

Published:2002-08 Issue:3-4 Volume:116 Page:325-359
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Mukhopadhyay Biswajit

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference53 articles.

1. Bailey, R.A., 1984. Chemical evolution and current state of the Long Valley magma chamber. In: Hill, D.P., Bailey, R.A., Ryall, A.S. (Eds.), Proc. Workshop XIX: Active Tectonic and Magmatic Processes beneath Long Valley Caldera, Eastern California. USGS Open-File Report 84-939, pp. 24–40.

2. Volcanism, structure, and geochronology of the Long Valley Caldera, Mono County, California;Bailey;J. Geophys. Res.,1976

3. Advective–diffusive transport of isotopic fronts: an example from Naxos, Greece;Bickle;Earth Planet. Sci. Lett.,1990

4. A transient model of the geothermal system of the long valley caldera, California;Blackwell;J. Geophys. Res.,1985

5. Isotope shift data and the natural evolution of geothermal systems;Blattner;Chem. Geol.,1985

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