The formation of SiO2-rich melts within the deep oceanic crust by hydrous partial melting of gabbros.

MLA

Koepke, Juergen, et al. “The Formation of SiO2-Rich Melts within the Deep Oceanic Crust by Hydrous Partial Melting of Gabbros.” Contributions to Mineralogy & Petrology, vol. 153, no. 1, Jan. 2007, pp. 67–84. EBSCOhost, https://doi.org/10.1007/s00410-006-0135-y.

APA

Koepke, J., Berndt, J., Feig, S. T., & Holtz, F. (2007). The formation of SiO2-rich melts within the deep oceanic crust by hydrous partial melting of gabbros. Contributions to Mineralogy & Petrology, 153(1), 67–84. https://doi.org/10.1007/s00410-006-0135-y

Chicago

Koepke, Juergen, Jasper Berndt, Sandrin T. Feig, and Francois Holtz. 2007. “The Formation of SiO2-Rich Melts within the Deep Oceanic Crust by Hydrous Partial Melting of Gabbros.” Contributions to Mineralogy & Petrology 153 (1): 67–84. doi:10.1007/s00410-006-0135-y.