Cite
Tectonic response of the central Chilean margin (35-38[degrees]S) to the collision and subduction of heterogeneous oceanic crust: a thermochronological study
MLA
Spikings, R., et al. “Tectonic Response of the Central Chilean Margin (35-38[Degrees]S) to the Collision and Subduction of Heterogeneous Oceanic Crust: A Thermochronological Study.” Journal of the Geological Society, vol. 165, no. 5, Sept. 2008, p. 941. 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.184643689&authtype=sso&custid=ns315887.
APA
Spikings, R., Dungan, M., Foeken, J., Carter, A., Page, L., & Stuart, F. (2008). Tectonic response of the central Chilean margin (35-38[degrees]S) to the collision and subduction of heterogeneous oceanic crust: a thermochronological study. Journal of the Geological Society, 165(5), 941.
Chicago
Spikings, R., M. Dungan, J. Foeken, A. Carter, L. Page, and F. Stuart. 2008. “Tectonic Response of the Central Chilean Margin (35-38[Degrees]S) to the Collision and Subduction of Heterogeneous Oceanic Crust: A Thermochronological Study.” Journal of the Geological Society 165 (5): 941. 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.184643689&authtype=sso&custid=ns315887.