Mechanisms of oxygen isotopic exchange and isotopic evolution of 18O/16O-depleted periclase zone marbles in the Alta aureole, Utah: insights from ion microprobe analysis of calcite-Reference-Cited by-同舟云学术

Mechanisms of oxygen isotopic exchange and isotopic evolution of 18O/16O-depleted periclase zone marbles in the Alta aureole, Utah: insights from ion microprobe analysis of calcite

Published:2008-08-20 Issue:1 Volume:157 Page:77-93
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Bowman John R.,Valley John W.,Kita Noriko T.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-008-0321-1.pdf

Reference58 articles.

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2. Ague JJ, Rye DM (1999) Simple models of CO2 release from metacarbonates with implications for interpretation of directions and magnitudes of fluid flow in the deep crust. J Petrol 40:1443–1462. doi: 10.1093/petrology/40.9.1443

3. Arita Y, Wada H (1990) Stable isotope evidence for migration of metamorphic fluids along grain boundaries of marbles. Geochem J 24:173–186

4. Baker AA, Calkins FC, Crittenden MD, Bromfield CS (1966) Geologic map of the Brighton quadrangle, Utah. U.S. Geological Survey Map GQ–535

5. Baumgartner LP, Valley JW (2001) Stable isotope transport and contact metamorphic fluid flow. In: Valley JW, Cole DR (eds) Stable isotope geochemistry. Reviews in mineralogy and geochemistry, vol 43. Mineralogical Soceity of America, Washington, DC, pp 415–468

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