Nature Communications (Nov 2022)

Vertical depletion of ophiolitic mantle reflects melt focusing and interaction in sub-spreading-center asthenosphere

  • Qing Xiong,
  • Hong-Kun Dai,
  • Jian-Ping Zheng,
  • William L. Griffin,
  • Hong-Da Zheng,
  • Li Wang,
  • Suzanne Y. O’ Reilly

DOI
https://doi.org/10.1038/s41467-022-34781-w
Journal volume & issue
Vol. 13, no. 1
pp. 1 – 11

Abstract

Read online

Upward depletion of ophiolitic mantle is produced by melt-peridotite reaction with lateral melt/rock ratio variations in an asthenospheric upwelling column, which flows to become the horizontal oceanic lithospheric mantle under spreading centers.