Peridotite-basalt association at MAR between 19°42′ and 19°59′ N: Evaluation of petrogenetic conditions and material balance during hydrothermal transformation of the oceanic crust.

MLA

Silantyev, S., et al. “Peridotite-Basalt Association at MAR between 19°42′ and 19°59′ N: Evaluation of Petrogenetic Conditions and Material Balance during Hydrothermal Transformation of the Oceanic Crust.” Petrology, vol. 23, no. 1, Jan. 2015, pp. 1–21. EBSCOhost, https://doi.org/10.1134/S0869591115010051.

APA

Silantyev, S., Krasnova, E., Bortnikov, N., Shatagin, K., Bychkova, Y., & Bel’tenev, V. (2015). Peridotite-basalt association at MAR between 19°42′ and 19°59′ N: Evaluation of petrogenetic conditions and material balance during hydrothermal transformation of the oceanic crust. Petrology, 23(1), 1–21. https://doi.org/10.1134/S0869591115010051

Chicago

Silantyev, S., E. Krasnova, N. Bortnikov, K. Shatagin, Ya. Bychkova, and V. Bel’tenev. 2015. “Peridotite-Basalt Association at MAR between 19°42′ and 19°59′ N: Evaluation of Petrogenetic Conditions and Material Balance during Hydrothermal Transformation of the Oceanic Crust.” Petrology 23 (1): 1–21. doi:10.1134/S0869591115010051.