Authors / CoAuthors
Smith, E.R.
Abstract
A reflection traverse was shot across the centre part of the Giralia Anticline in the Carnarvon Basin of Western Australia, in an attempt to verify the unconformity between Mesozoic and Palaeozoic sediments shown by a previous traverse across the northern part of the anticline. Shallow seismic events recorded were of good quality and correlated very well with surface geology. They also indicated two faults in places where steep dips in surface beds might, by analogy with the northern end, be expected. Deep events were in general of poor quality and inconsistent. However, over approximately a mile of the traverse, they were of good quality and indicated nonconformity with the shallow events.
Product Type
document
eCat Id
9084
Contact for the resource
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Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
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2601
Australia
Keywords
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- GA PublicationRecord
- ( Theme )
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- seismics
- ( Theme )
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- seismic reflection
- ( Theme )
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- geology
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- AU-WA
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_External
Publication Date
1954-01-01T00:00:00
Creation Date
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unknown
Topic Category
geoscientificInformation
Series Information
Record 1954/067
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Legacy product, lineage not available
Parent Information
Extents
[-23.7, -22.4, 113.8, 114.5]
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