In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 124, No. 11 ( 2019-11), p. 11866-11899
Abstract:
Magnetic quiet zone in the continental slope is induced by thick Mesozoic strata, not by large‐scale mantle exhumation or demagnetization Magmatic underplating caused multiple isolated lower crust high‐velocity zones but not a single high‐velocity layer Deep mantle upwelling and serpentinization occurred at the continent‐ocean boundary
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1029/2019JB017785
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13
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