In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 128, No. 4 ( 2023-04)
Kurzfassung:
The upper mantle beneath the Changbaishan volcano is characterized by two seismic low‐velocity anomalies The shallow low‐velocity anomaly (i.e., shallow than 370 km, with a higher Vp/Vs ratio) is due to partial melting The deep anomaly (i.e., atop the 410‐km, with a lower Vp/Vs ratio) is likely caused by the moduli reduction during the phase transformation
Materialart:
Online-Ressource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1029/2022JB025671
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2023
ZDB Id:
2016813-5
ZDB Id:
161666-3
ZDB Id:
3094197-0
SSG:
16,13