Stable chlorine isotope behavior during volcanic degassing of H2O and CO2 at Mono Craters, CA-Reference-Cited by-同舟云学术

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Stable chlorine isotope behavior during volcanic degassing of H2O and CO2 at Mono Craters, CA

Published:2014-02-19 Issue:3 Volume:76 Page:
ISSN:0258-8900
Container-title:Bulletin of Volcanology
language:en
Short-container-title:Bull Volcanol

Author:

Barnes Jaime D.,Prather Timothy J.,Cisneros Miguel,Befus Kenneth,Gardner James E.,Larson Toti E.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

http://link.springer.com/content/pdf/10.1007/s00445-014-0805-y.pdf

Reference72 articles.

1. Achauer U, Greene L, Evans JR, Iyer HM (1986) Nature of the magma chamber underlying the Mono Craters area, Eastern California, as determined from teleseismic travel time residuals. J Geophys Res 91:13873–13891

2. Aiuppa A, Baker DR, Webster JD (2009) Halogens in volcanic systems. Chem Geol 263:1–18

3. Anderson AT, Newman S, Williams SN, Druitt TH, Skirius C, Stolper E (1989) H2O, C02, CI, and gas in Plinian and ash-flow Bishop rhyolite. Geology 17:221–225

4. Arcuri T, Brimhall G (2003) The chloride source for atacamite mineralization at the Radomiro Tomic porphyry copper deposit, northern Chile. Econ Geol 98:1667–1681

5. Bai TB, Koster van Groos AF (1994) Diffusion of chlorine in granitic melts. Geochim Cosmochim Acta 58:113–123

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