Regional correlation of mesoproterozoic structures and deformational events in the Albany-Fraser orogen, Western Australia

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Abstract

Geologic mapping and meso- and microstructural analysis of a previously unstudied area in the western part of the Mesoproterozoic Albany-Fraser orogen, Western Australia, leads to a correlation of deformational events along the exposed length of the orogen. The earliest deformational event (D1) accompanied granulite-facies metamorphism and is characterized by a locally preserved subhorizontal foliation and associated recumbent folds. This event is interpreted to record northwest-southeast contraction. The second event (D2) produced a subvertical, east-northeaststriking foliation and variably plunging, upright folds. Northwest-vergent folds (toward 333°) and sparse kinematic indicators suggest southeast-up tectonic transport with a dextral component of movement. A third deformational event (D3) is manifested by a conjugate set of mylonitic to cataclastic shear zones with a dominant, dextral set oriented at 105° and a subordinate, sinistral set oriented at 010°. The bisector of the average orientations for the shear zones is 325°, consistent with northwest-southeast shortening. Like the D2 structures, the D3 structures may represent deformation in a dextral transpressive setting. D4 structures include two subvertical joint sets, one oriented at 355° and the other at 105°. All structures are similar in geometry and kinematics to structures near Albany, which have been constrained to 1190-1170 Ma (Precambrian Res., 59 (1992) 95), as well as structures east of Esperance that are associated with a major tectonothermal event at 1345-1260 Ma (Precambrian Res., 102 (2000) 155). Additional geochronological data, particularly from the Western Albany-Fraser orogen, are needed to resolve this apparent discrepancy. There is a near one-to-one correlation in lithology, structural style, metamorphic grade, kinematics, and possibly timing of deformational events between the Albany-Fraser orogen and the Bunger Hills of East Antarctica, supporting the previously suggested ties between these two areas. Marked dissimilarities, however, in model TDM ages, U-Pb zircon dates, kinematics and timing of deformation, and timing of metamorphism between the Albany-Fraser orogen and the Oaxacan Complex of southern Mexico raise serious doubts regarding the viability of Rodinia reconstructions that juxtapose those two Mesoproterozoic terranes.

Original languageEnglish (US)
Pages (from-to)129-154
Number of pages26
JournalPrecambrian Research
Volume116
Issue number1-2
DOIs
StatePublished - May 31 2002

Fingerprint

Kinematics
kinematics
fold
foliation
shear zone
Precambrian
metamorphism
Time division multiplexing
Rodinia
Lithology
Tectonics
granulite facies
contraction
terrane
lithology
viability
zircon
geometry
tectonics
Geometry

Keywords

  • Albany-Fraser orogen
  • Australia
  • Mesoproterozoic
  • Rodinia
  • Tectonics

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geology

Cite this

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title = "Regional correlation of mesoproterozoic structures and deformational events in the Albany-Fraser orogen, Western Australia",
abstract = "Geologic mapping and meso- and microstructural analysis of a previously unstudied area in the western part of the Mesoproterozoic Albany-Fraser orogen, Western Australia, leads to a correlation of deformational events along the exposed length of the orogen. The earliest deformational event (D1) accompanied granulite-facies metamorphism and is characterized by a locally preserved subhorizontal foliation and associated recumbent folds. This event is interpreted to record northwest-southeast contraction. The second event (D2) produced a subvertical, east-northeaststriking foliation and variably plunging, upright folds. Northwest-vergent folds (toward 333°) and sparse kinematic indicators suggest southeast-up tectonic transport with a dextral component of movement. A third deformational event (D3) is manifested by a conjugate set of mylonitic to cataclastic shear zones with a dominant, dextral set oriented at 105° and a subordinate, sinistral set oriented at 010°. The bisector of the average orientations for the shear zones is 325°, consistent with northwest-southeast shortening. Like the D2 structures, the D3 structures may represent deformation in a dextral transpressive setting. D4 structures include two subvertical joint sets, one oriented at 355° and the other at 105°. All structures are similar in geometry and kinematics to structures near Albany, which have been constrained to 1190-1170 Ma (Precambrian Res., 59 (1992) 95), as well as structures east of Esperance that are associated with a major tectonothermal event at 1345-1260 Ma (Precambrian Res., 102 (2000) 155). Additional geochronological data, particularly from the Western Albany-Fraser orogen, are needed to resolve this apparent discrepancy. There is a near one-to-one correlation in lithology, structural style, metamorphic grade, kinematics, and possibly timing of deformational events between the Albany-Fraser orogen and the Bunger Hills of East Antarctica, supporting the previously suggested ties between these two areas. Marked dissimilarities, however, in model TDM ages, U-Pb zircon dates, kinematics and timing of deformation, and timing of metamorphism between the Albany-Fraser orogen and the Oaxacan Complex of southern Mexico raise serious doubts regarding the viability of Rodinia reconstructions that juxtapose those two Mesoproterozoic terranes.",
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N2 - Geologic mapping and meso- and microstructural analysis of a previously unstudied area in the western part of the Mesoproterozoic Albany-Fraser orogen, Western Australia, leads to a correlation of deformational events along the exposed length of the orogen. The earliest deformational event (D1) accompanied granulite-facies metamorphism and is characterized by a locally preserved subhorizontal foliation and associated recumbent folds. This event is interpreted to record northwest-southeast contraction. The second event (D2) produced a subvertical, east-northeaststriking foliation and variably plunging, upright folds. Northwest-vergent folds (toward 333°) and sparse kinematic indicators suggest southeast-up tectonic transport with a dextral component of movement. A third deformational event (D3) is manifested by a conjugate set of mylonitic to cataclastic shear zones with a dominant, dextral set oriented at 105° and a subordinate, sinistral set oriented at 010°. The bisector of the average orientations for the shear zones is 325°, consistent with northwest-southeast shortening. Like the D2 structures, the D3 structures may represent deformation in a dextral transpressive setting. D4 structures include two subvertical joint sets, one oriented at 355° and the other at 105°. All structures are similar in geometry and kinematics to structures near Albany, which have been constrained to 1190-1170 Ma (Precambrian Res., 59 (1992) 95), as well as structures east of Esperance that are associated with a major tectonothermal event at 1345-1260 Ma (Precambrian Res., 102 (2000) 155). Additional geochronological data, particularly from the Western Albany-Fraser orogen, are needed to resolve this apparent discrepancy. There is a near one-to-one correlation in lithology, structural style, metamorphic grade, kinematics, and possibly timing of deformational events between the Albany-Fraser orogen and the Bunger Hills of East Antarctica, supporting the previously suggested ties between these two areas. Marked dissimilarities, however, in model TDM ages, U-Pb zircon dates, kinematics and timing of deformation, and timing of metamorphism between the Albany-Fraser orogen and the Oaxacan Complex of southern Mexico raise serious doubts regarding the viability of Rodinia reconstructions that juxtapose those two Mesoproterozoic terranes.

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