Complex continental growth along the proto-Pacific margin of East Gondwana

Nicholas Rawlinson, Pierre Arroucau, Robert Musgrave, Ross Cayley, Mallory Young, Michelle Salmon

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

We use ambient noise recordings from the largest transportable seismic array in the Southern Hemisphere to image azimuthal variations in Rayleigh wave phase anisotropy in the crust beneath southeast Australia. This region incorporates a transition from the Precambrian shield region of Australia in the west to younger Phanerozoic terranes in the east, which are thought to have been formed by subduction-accretion processes. Our results, which span the shallow to lower crust, show a strong and consistent pattern of anisotropy that is oriented north-south, approximately parallel to the former margin of East Gondwana. However, significant deviations from this trend persist through the period range 2.5 s to >10 s. One of the most notable deviations occurs along the edge of cratonic Australia, where the Curnamona Province forms a salient into the younger accretionary terrane; here, the fast axis of anisotropy follows the boundary almost exactly, and is virtually coincident with magnetic lineations extracted from aeromagnetic data. To the east of this boundary beneath the Lachlan orogen, a region masked by the Cenozoic Murray Basin, the fast axis of anisotropy becomes strongly curved and traces out a semicircular pattern with a radius of 200–250 km. Farther east, the fast axis of anisotropy returns to a dominantly north-south orientation. These new findings provide strong observational support to recent geodynamic modeling results that demonstrate how large-scale oroclinal structures can become embedded in accretionary mountain belts.
Original languageEnglish
Pages (from-to)783-786
Number of pages4
JournalGeology
Volume42
Issue number9
Early online date21 Jul 2014
DOIs
Publication statusPublished - Sep 2014

Fingerprint

Gondwana
anisotropy
terrane
ambient noise
aeromagnetic survey
Rayleigh wave
lineation
Phanerozoic
lower crust
geodynamics
Southern Hemisphere
shield
Precambrian
subduction
accretion
crust
mountain
basin
modeling
young

Keywords

  • seismology
  • tectonics
  • tomography
  • Australia
  • crustal anisotropy

Cite this

Rawlinson, N., Arroucau, P., Musgrave, R., Cayley, R., Young, M., & Salmon, M. (2014). Complex continental growth along the proto-Pacific margin of East Gondwana. Geology, 42(9), 783-786. https://doi.org/10.1130/G35766.1

Complex continental growth along the proto-Pacific margin of East Gondwana. / Rawlinson, Nicholas; Arroucau, Pierre; Musgrave, Robert; Cayley, Ross ; Young, Mallory; Salmon, Michelle.

In: Geology, Vol. 42, No. 9, 09.2014, p. 783-786.

Research output: Contribution to journalArticle

Rawlinson, N, Arroucau, P, Musgrave, R, Cayley, R, Young, M & Salmon, M 2014, 'Complex continental growth along the proto-Pacific margin of East Gondwana', Geology, vol. 42, no. 9, pp. 783-786. https://doi.org/10.1130/G35766.1
Rawlinson N, Arroucau P, Musgrave R, Cayley R, Young M, Salmon M. Complex continental growth along the proto-Pacific margin of East Gondwana. Geology. 2014 Sep;42(9):783-786. https://doi.org/10.1130/G35766.1
Rawlinson, Nicholas ; Arroucau, Pierre ; Musgrave, Robert ; Cayley, Ross ; Young, Mallory ; Salmon, Michelle. / Complex continental growth along the proto-Pacific margin of East Gondwana. In: Geology. 2014 ; Vol. 42, No. 9. pp. 783-786.
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