A Partial Molten Low‐Velocity Layer Atop the Mantle Transition Zone Beneath the Western Junggar: Implication for the Formation of Subduction‐Induced Sub‐Slab Mantle Plume

• Published in: Geochemistry, Geophysics, Geosystems
• Main Authors: Guohui Li, Yuanze Zhou, Lin Ding, Yuan Gao, Ling Bai, Heng Zhang, Le Hu, Zhengyang Pan, Changhui Ju, Dingding Zhang
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2022
• Subjects: low‐velocity layer; mantle transition zone; triplicated waveform modeling; plate subduction; mantle plume; western Junggar; Geophysics. Cosmic physics; QC801-809; Geology; QE1-996.5; Ocean Island; Siberia
• Online Access: https://doi.org/10.1029/2021GC010150; https://doaj.org/article/6e2872eaa1514a72a7c613a3e1c7a809

Abstract Deep subduction of plate generally could induce a partial molten low‐velocity layer (LVL) atop the mantle transition zone (MTZ) around the subduction zone. But the effects of the LVL to its upper lithosphere are less known, especially at the oceanward direction of subducted slab. Here, we image the seismic velocity structure atop the MTZ by matching the synthetics and the observed triplicated P‐ and SH‐wave waveforms recorded by Xinjiang seismic network from four earthquakes in the southwestern Siberia. Our observations reveal a partial molten LVL atop the MTZ beneath the western Junggar (WJ) in the southwestern Central Asian Orogenic Belt. The SH‐wave velocity drop for the LVL is −5.6% which is larger than −4.4% of the P‐wave when its thickness is 29 km. It is inferred that the subducted Paleo‐Asian oceanic plate induces hydrous MTZ materials underneath the subducted slab to upwell to the upper mantle, and form the partial molten LVL. Combined with previous geophysical and geological results, we propose a new geodynamical process involving the lithosphere and MTZ underneath the subducted slab: the melt in the LVL is likely to upwell through slab window, which could be triggered by mid‐oceanic ridge subduction or self‐sustained buoyancy. This mode could account for the contemporaneous break‐off fossil oceanic plate, ocean island basalts‐type rocks, extensive A‐type granitoids, adakite, and porphyry Cu‐Au in the WJ during the late Carboniferous to early Permian.