Library Open Repository

Nature of the continent-ocean transition on the non-volcanic rifted margin of the central Great Australian Bight

Downloads

Downloads per month over past year

Sayers, J and Symonds, PA and Direen, NG and Bernadel, G (2001) Nature of the continent-ocean transition on the non-volcanic rifted margin of the central Great Australian Bight. In: Non-Volcanic Rifting of Continental Margins: A Comparison of Evidence from Land and Sea. Geological Society special publication (187). Geological Society of London, London, pp. 51-76. ISBN 1862390916

[img] PDF
Sayers_etal_01_GSLSP187_GAB.pdf | Request a copy
Full text restricted
Available under University of Tasmania Standard License.

Abstract

A region of 50- 120km width defines the continent-ocean transition (COT) in the central Great Australian Bight. It is characterized by a thin apron of post-break-up sediments overlying complexly deformed sediments and intruded crust bounded landward by a basement ridge complex and oceanward by rough oceanic basement. Recently acquired deep reflection and refraction seismic data have significantly enhanced understanding of the COT and basement ridge. Modelled gravity and magnetic data, and features interpreted from seismic data, are consistent with aspects of extensional and break-up models proposed for the West Iberia margin. Many of the features and relationships observed beneath the outer margin of the central Great Australian Bight can be explained by extension within a lithosphere-scale 'pure-shear' environment involving four layers: brittle upper crust and upper mantle, and ductile lower crust and lower lithospheric mantle. The COT is interpreted to be underlain by extended continental lithosphere. Thus, the continentocean boundary is unequivocally defined between oceanic crust and the COT and appears to be associated with sea-floor spreading magnetic anomaly 33, indicating that break-up and sea-floor spreading did not commence until c. 83 Ma (early Carnpanian time), later than the currently accepted 95Ma age. The major part of the basement ridge complex is probably a combination of serpentinized peridotites and mafic intrusions or extrusions derived by mantle upwelling and limited partial melting. The magmatic products of this process probably cooled during chron 34 producing a distinctive magnetic anomaly, but one that does not relate to break-up and sea-floor spreading.

Item Type: Book Section
Publisher: Geological Society of London
Page Range: pp. 51-76
Identification Number - DOI: 10.1144/GSL.SP.2001.232.01.28
Date Deposited: 07 Sep 2010 05:53
Last Modified: 18 Nov 2014 04:12
URI: http://eprints.utas.edu.au/id/eprint/10033
Item Statistics: View statistics for this item

Repository Staff Only (login required)

Item Control Page Item Control Page