Authors / CoAuthors
Jones, L.E.A.
Abstract
Steeply dipping reflectors have been recognised on stack data for the Lachlan Fold Belt (up to 60º) and the Tanami Province (up to 70º), demonstrating that significant dip filtering does not occur during acquisition with regional parameters. DMO correction is essential during processing to correctly image such features. These events appear to be real reflections not reflected refractions or diffractions, as proved by analysis of amplitude, frequency and moveout on shot records. In the Tanami case, the reflection is related to a small circular feature in the potential field image, possibly the expression of a granite stock. Migration proved problematical, as most migration algorithms could not simultaneously migrate the steep dips and remain artefact free in other parts of the section, suggesting that interpretation must be done on multiple sections in such cases.
Product Type
nonGeographicDataset
eCat Id
64785
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Custodian
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Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
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Australia
Keywords
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- External PublicationAbstract
- ( Theme )
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- seismology
- ( Theme )
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- seismic sections
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- AU
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_Internal
Publication Date
2006-01-01T00:00:00
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geoscientificInformation
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Unknown
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Extents
[-35.0, -19.0, 127.0, 150.0]
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