Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time

MLA

Stern, Robert J. “Evidence from Ophiolites, Blueschists, and Ultrahigh-Pressure Metamorphic Terranes That the Modern Episode of Subduction Tectonics Began in Neoproterozoic Time.” Geology, vol. 33, no. 7, July 2005, p. 557. 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.133864082&authtype=sso&custid=ns315887.

APA

Stern, R. J. (2005). Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time. Geology, 33(7), 557.

Chicago

Stern, Robert J. 2005. “Evidence from Ophiolites, Blueschists, and Ultrahigh-Pressure Metamorphic Terranes That the Modern Episode of Subduction Tectonics Began in Neoproterozoic Time.” Geology 33 (7): 557. 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.133864082&authtype=sso&custid=ns315887.