O isotope zoning in garnet and staurolite: evidence for closed-system mineral growth during regional metamorphism

MLA

Kohn, Matthew J., et al. “O Isotope Zoning in Garnet and Staurolite: Evidence for Closed-System Mineral Growth during Regional Metamorphism.” American Mineralogist, vol. 78, no. 9–10, Sept. 1993, p. 988. EBSCOhost, widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsggo&AN=edsgcl.14777455&authtype=sso&custid=ns315887.

APA

Kohn, M. J., Valley, J. W., Elsenheimer, D., & Spicuzza, M. J. (1993). O isotope zoning in garnet and staurolite: evidence for closed-system mineral growth during regional metamorphism. American Mineralogist, 78(9–10), 988.

Chicago

Kohn, Matthew J., John W. Valley, Don Elsenheimer, and Michael J. Spicuzza. 1993. “O Isotope Zoning in Garnet and Staurolite: Evidence for Closed-System Mineral Growth during Regional Metamorphism.” American Mineralogist 78 (9–10): 988. http://widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsggo&AN=edsgcl.14777455&authtype=sso&custid=ns315887.