In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 23, No. 11 ( 2022-11)
Abstract:
A bathymetry map was constructed for Valdivia Bank from multibeam data merged with satellite altimetry‐predicted depths Valdivia Bank experienced extension, forming rifts, and secondary volcanism, uplift, and exposure, then was capped by carbonate sediments Valdivia Bank shows evidence of mass wasting, partly triggered by Cenozoic uplift and erosion, but also owing to sediment cap instability
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2022GC010624
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2022
detail.hit.zdb_id:
2027201-7
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