Cite
High temperature (>800°C) brine phase present during the formation of Northern Bushveld magmatic sulfide Cu-Ni-PGE deposits
MLA
Jacob J. Hanley, et al. “High Temperature (>800°C) Brine Phase Present during the Formation of Northern Bushveld Magmatic Sulfide Cu-Ni-PGE Deposits.” Goldschmidt2021 Abstracts, Jan. 2021. 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=edsair&AN=edsair.doi...........d1e38d602eb7509c15867e7ace048fc3&authtype=sso&custid=ns315887.
APA
Jacob J. Hanley, Iain McDonald, Marina A. Yudovskaya, Katie McFall, Judith A. Kinnaird, Brian Tattitch, & Mitchell J. Kerr. (2021). High temperature (>800°C) brine phase present during the formation of Northern Bushveld magmatic sulfide Cu-Ni-PGE deposits. Goldschmidt2021 Abstracts.
Chicago
Jacob J. Hanley, Iain McDonald, Marina A. Yudovskaya, Katie McFall, Judith A. Kinnaird, Brian Tattitch, and Mitchell J. Kerr. 2021. “High Temperature (>800°C) Brine Phase Present during the Formation of Northern Bushveld Magmatic Sulfide Cu-Ni-PGE Deposits.” Goldschmidt2021 Abstracts, January. 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=edsair&AN=edsair.doi...........d1e38d602eb7509c15867e7ace048fc3&authtype=sso&custid=ns315887.