中源地震脱水脆变机制的岩石学研究进展
The Advance of Petrologic Mechanism of Dehydration Embrittlement in Intermediate-depth Earthquakes
Fig. 7 Mn and Mg content chemical maps of garnet from lawsonite eclogites in Monviso ophiolite, Western Alps The garnet shows presence of two main garnet generations: first one exhibits Mn-rich growth, and second is characterized by Mg-rich overgrowth and healed fossilized fracture networks which imply fossil earthquakes [ 39 ]
