In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 19, No. 2 ( 2018-02), p. 356-378
Abstract:
Mapping the surface of Venere mud volcano and surrounding Squillace Canyon reveals details of mudflow morphologies and channel bedforms Ages of mudflows are determined by sediment cores and tephrochronology and reveal the mud volcano evolution during the last 4,000 years Mobile mudflows are documented and suggest Venere mud volcano to be the most active structure in the Calabrian Accretionary Prism
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1002/2017GC007166
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2018
detail.hit.zdb_id:
2027201-7