%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Denèle, Y.
%A Roques, D.
%A Ganne, Jérôme
%A Chardon, Dominique
%A Rousse, Sonia
%A Barbey, P.
%T Strike-slip metamorphic core complexes : gneiss domes emplaced in releasing bends
%D 2017
%L fdi:010071233
%G ENG
%J Geology
%@ 0091-7613
%K OMAN ; ARABIQUE PENINSULE
%M ISI:000411705800015
%N 10
%P 903-906
%R 10.1130/g39065.1
%U https://www.documentation.ird.fr/hor/fdi:010071233
%> https://www.documentation.ird.fr/intranet/publi/2017/10/010071233.pdf
%V 45
%W Horizon (IRD)
%X We investigate the development of a Neoproterozoic metamorphic core complex (MCC) in the Marbat area (southern Arabian Peninsula). The MCC is a gneiss dome emplaced in a releasing bend along a dextral strike-slip fault system. Dome emplacement-related extension was at a high angle to the long axis of the dome and 65 degrees from the strike-slip fault system. Shortening is recorded in the upper plate of the MCC in a direction normal to the extension direction. Extensional emplacement of the gneiss dome accommodated lower crust exhumation and contributed to the formation of a ductile strike-slip releasing bend from an initial fault step. The Marbat example allows defining transversal stretching-dominated strike-slip MCCs, which would represent the early development stages of longitudinal stretching-dominated strike-slip MCCs. Conversely, longitudinal stretching-dominated strike-slip MCCs produced at low finite extension would result from strike-slip-dominated transtension. This study bears important implications for lower crust exhumation under pulla-part basin systems in obliquely convergent or divergent settings.
%$ 064 ; 066