In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 47, No. 9 ( 2020-05-16)
Abstract:
We provide the first evidence for the presence of HIMU component in the magma source Subduction‐related, carbonatite‐metasomatized mantle is a likely candidate for the HIMU reservoir The transition zone may be an important reservoir in the development of mantle heterogeneities
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2020GL087260
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13