Professor Yao Huajian’s research group from the School of Earth and Space Sciences of the University of Science and Technology of China (USTC), in cooperation with Dr. Piero Poli from Grenoble-Alpes University of France, combined the unique resolution reflected body waves (P410P and P660P) retrieved from ambient noise interferometry with mineral physics modeling, to shed new light on transition zone physics. Their work was published in Nature Communications.
Click here for original story, Direct evidence of segregated oceanic crust trapped within the mantle transition zone
Source: Phys.org