@article{fdi:010071233,
  title = {{S}trike-slip metamorphic core complexes : gneiss domes emplaced in releasing bends},
  author = {{D}en{\`e}le, {Y}. and {R}oques, {D}. and {G}anne, {J}{\'e}r{\^o}me and {C}hardon, {D}ominique and {R}ousse, {S}onia and {B}arbey, {P}.},
  editor = {},
  language = {{ENG}},
  abstract = {{W}e investigate the development of a {N}eoproterozoic metamorphic core complex ({MCC}) in the {M}arbat area (southern {A}rabian {P}eninsula). {T}he {MCC} is a gneiss dome emplaced in a releasing bend along a dextral strike-slip fault system. {D}ome emplacement-related extension was at a high angle to the long axis of the dome and 65 degrees from the strike-slip fault system. {S}hortening is recorded in the upper plate of the {MCC} in a direction normal to the extension direction. {E}xtensional 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. {T}he {M}arbat example allows defining transversal stretching-dominated strike-slip {MCC}s, which would represent the early development stages of longitudinal stretching-dominated strike-slip {MCC}s. {C}onversely, longitudinal stretching-dominated strike-slip {MCC}s produced at low finite extension would result from strike-slip-dominated transtension. {T}his study bears important implications for lower crust exhumation under pulla-part basin systems in obliquely convergent or divergent settings.},
  keywords = {{OMAN} ; {ARABIQUE} {PENINSULE}},
  booktitle = {},
  journal = {{G}eology},
  volume = {45},
  numero = {10},
  pages = {903--906},
  ISSN = {0091-7613},
  year = {2017},
  DOI = {10.1130/g39065.1},
  URL = {https://www.documentation.ird.fr/hor/fdi:010071233},
}