In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 123, No. 3 ( 2018-03), p. 2090-2114
Abstract:
We image a two‐layered thin crust within the Ionian basin that we interpreted to be of probable oceanic origin The deep structure of the Malta Escarpment shows an abrupt crustal thinning zone that is interpreted to result from a transform origin of the margin The major tear fault accommodating the slab roll back of the subduction along the eastern Sicily margin was located along the Alfeo‐Fault System
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1002/2017JB015312
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2018
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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