In:
Tectonics, American Geophysical Union (AGU), Vol. 39, No. 3 ( 2020-03)
Abstract:
The reactivation of the Subduction Tear Edge Propagator fault zone on the southern edge of the Alboran Domain forms the South Alboran Ridge The style of the present‐day structure of the South Alboran region implies an interaction between thick‐skinned and thin‐skinned tectonics Undercompacted shales and inherited crustal structures are involved in the structural evolution of the South Alboran Basin
Type of Medium:
Online Resource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1029/2019TC005885
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
2013221-9
detail.hit.zdb_id:
780264-X
SSG:
16,13
SSG:
13
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