U-Pb zircon geochronology of eclogites from the Scandian Orogen, northern Western Gneiss Region, Norway: 14-20 million years between eclogite crystallization and return to amphibolite-facies conditions.

MLA

Krogh, Thomas E., et al. “U-Pb Zircon Geochronology of Eclogites from the Scandian Orogen, Northern Western Gneiss Region, Norway: 14-20 Million Years between Eclogite Crystallization and Return to Amphibolite-Facies Conditions.” Canadian Journal of Earth Sciences, vol. 48, no. 2, Feb. 2011, pp. 441–72. 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=edb&AN=59164639&authtype=sso&custid=ns315887.

APA

Krogh, T. E., Kamo, S. L., Robinson, P., Terry, M. P., & Kwok, K. (2011). U-Pb zircon geochronology of eclogites from the Scandian Orogen, northern Western Gneiss Region, Norway: 14-20 million years between eclogite crystallization and return to amphibolite-facies conditions. Canadian Journal of Earth Sciences, 48(2), 441–472.

Chicago

Krogh, Thomas E., Sandra L. Kamo, Peter Robinson, Michael P. Terry, and Kim Kwok. 2011. “U-Pb Zircon Geochronology of Eclogites from the Scandian Orogen, Northern Western Gneiss Region, Norway: 14-20 Million Years between Eclogite Crystallization and Return to Amphibolite-Facies Conditions.” Canadian Journal of Earth Sciences 48 (2): 441–72. 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=edb&AN=59164639&authtype=sso&custid=ns315887.