Authors / CoAuthors
Finlayson, D.M. | Prodehl, C. | Collins, C.D.N.
Abstract
The interpreted velocity-depth structure in the crust of the Lachlan Fold Belt in southeastern Australia indicates that velocity gradients, rather than discontinuous velocity changes, characterise the region. The velocity-depth morphology varies across the region. In the upper crust at depths less than 12 km, there is evidence in three areas for velocity decreases within a general velocity increase from about 5.6 km/s to 6.3 km/s. In the middle crust (depth range 16 km to about 35 km) a low velocity zone is interpreted within a general increase in velocity from 6.3 km/s to greater than 7 km/s; the prominence of the low velocity zone varies throughout the region. The upper mantle velocity is in the range 8.02 to 8.05 km/s; this velocity is reached at a depth slightly greater than 50 km under the highest topography in Australia, and at depths between 40 and 50 km elsewhere. There are similarities between the velocity-depth structure in southeastern Australia and that in the Appalachian Orogen of North America. Geochemical mixing and/or compositional inhomogeneity is a likely reason for the velocity-depth structures, and such inhomogeneity is probably still influencing current moderate earthquake activity and continuing highland uplift. In pre-Ordovician times the region of the Lachlan Fold Belt probably consisted of continental crust which was submerged and thickened by episodic crustal development similar to the processes which resulted in the Appalachian Orogen.
Product Type
document
eCat Id
81004
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Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
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Keywords
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- GA PublicationJournal
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- NSWVIC
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_External
Publication Date
1979-01-01T00:00:00
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geoscientificInformation
Series Information
BMR Journal of Australian Geology and Geophysics 4:3:243-252
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Unknown
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Extents
[-37.0, -32.0, 146.0, 152.0]
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