@article{fdi:010083755,
  title = {{S}train partitioning and exhumation in oblique {T}aiwan collision : role of rift architecture and plate kinematics},
  author = {{C}onand, {C}. and {M}outhereau, {F}. and {G}anne, {J}{\'e}r{\^o}me and {T}ien {S}hun {L}in, {A}. and {L}ahfid, {A}. and {D}audet, {M}. and {M}esalles, {L}. and {G}iletycz, {S}. and {B}onzani, {M}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}aiwan is an archetypal example of continental accretionary wedges. {Y}et the generally poor knowledge of three-dimensional strain distribution over time and role of architecture of the rifted margin shed doubt on the cylindrical two-dimensional kinematic models of {T}aiwan collision. {H}ere we provide new field-based constraints on strain distribution, new {R}aman {S}pectroscopy on {C}arbonaceous {M}aterials temperatures and apply mica-chlorite multiequilibrium approach to determine pressure-temperature in the {C}entral {R}ange of {T}aiwan. {W}e identify three distinct structural domains that define zones of orthogonal shortening in the western {B}ackbone {R}ange and left-lateral ductile shearing overprinted by left-lateral transtensional brittle deformation in eastern {C}entral {R}ange. {F}ield surveys show the lack of nappe stacking in the {B}ackbone {R}ange. {C}ombining new temperature estimates with existing thermochronological constraints we emphasize that western {T}aiwan mostly inherited preorogenic thermal history. {W}e show that metamorphic peak conditions of 5-6 kbar and 330-400 °{C} in the eastern {B}ackbone {R}ange and {HP} rocks of the {Y}uli {B}elt exhumed along the {P}-{T} paths related to transcurrent deformation. {W}e propose a three-dimensional kinematic model of {T}aiwan accounting for the oblique motion of the {P}hilippine {S}ea {P}late relative to the plate boundary and the reactivation of a {NS} striking transform fault in the {S}outh {C}hina {S}ea rifted margin. {R}ecent and ongoing strain partitioning in the {T}aiwan accretionary wedge is reflected by the coexistence of brittle left-lateral shear, oblique extension, and contraction. {O}ur results have impact on orogen-based plate kinematic reconstructions that consider two-dimensional kinematic evolution of orogens},
  keywords = {{TAIWAN} ; {MER} {DE} {CHINE} ; {HENGCHUN} {PENINSULE}},
  booktitle = {},
  journal = {{T}ectonics},
  volume = {39},
  numero = {4},
  pages = {e2019{TC}005798 [30 ]},
  ISSN = {0278-7407},
  year = {2020},
  DOI = {10.1029/2019{TC}005798},
  URL = {https://www.documentation.ird.fr/hor/fdi:010083755},
}