In:
Tectonics, American Geophysical Union (AGU), Vol. 39, No. 11 ( 2020-11)
Abstract:
We present the seismostratigraphic analysis of the last ~1.8 Ma tectonosedimentary evolution of the north Tunisian continental margin Individual Quaternary depocenters developed syntectonic to faulting, and faulting influenced sedimentation patterns We identify an abrupt variation of sedimentation rates coeval to a change in the strata geometry of the units near faults at 402 ± 5 ka
Type of Medium:
Online Resource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1029/2020TC006243
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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