Cite
A low-velocity layer atop the mantle transition zone beneath the western Central Asian Orogenic Belt: Upper mantle melting induced by ancient slab subduction.
MLA
Li, Guohui, et al. “A Low-Velocity Layer atop the Mantle Transition Zone beneath the Western Central Asian Orogenic Belt: Upper Mantle Melting Induced by Ancient Slab Subduction.” Earth & Planetary Science Letters, vol. 578, Jan. 2022, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.epsl.2021.117287.
APA
Li, G., Gao, Y., Zhou, Y., Ju, C., Shi, Y., & Cui, Q. (2022). A low-velocity layer atop the mantle transition zone beneath the western Central Asian Orogenic Belt: Upper mantle melting induced by ancient slab subduction. Earth & Planetary Science Letters, 578, N.PAG. https://doi.org/10.1016/j.epsl.2021.117287
Chicago
Li, Guohui, Yuan Gao, Yuanze Zhou, Changhui Ju, Yutao Shi, and Qinghui Cui. 2022. “A Low-Velocity Layer atop the Mantle Transition Zone beneath the Western Central Asian Orogenic Belt: Upper Mantle Melting Induced by Ancient Slab Subduction.” Earth & Planetary Science Letters 578 (January): N.PAG. doi:10.1016/j.epsl.2021.117287.