Evolution of Olivine Fabrics During Deep Subduction and Exhumation of Continental Crust: Insights From the Yinggelisayi Garnet Lherzolite, South Altyn, NW China

Abstract

Olivine fabrics are described in terms of their relationship to the crystallographic framework (x, y, and z axes), and can provide important information for understanding the evolution of the upper mantle, mantle flow pattern, mantle dynamics and tectonics (