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dc.contributor.authorBona, Andrej
dc.contributor.authorNadri, D.
dc.contributor.authorBrajanovski, Miroslav
dc.date.accessioned2017-01-30T12:01:07Z
dc.date.available2017-01-30T12:01:07Z
dc.date.created2011-03-10T20:01:21Z
dc.date.issued2010
dc.identifier.citationBona, Andrej and Nadri, Dariush and Brajanovski, Miroslav. 2010. Thomsen's parameters from p-wave measurements in a spherical sample. Geophysical Prospecting. 60 (1): pp. 103-116.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/17333
dc.identifier.doi10.1111/j.1365-2478.2010.00917.x
dc.description.abstract

The aim of this paper is to understand the seismic anisotropy of the overburden shale in an oilfield in the North West Shelf of Western Australia. To this end, we first find the orientation of the symmetry axis of a spherical shale sample from measurements of ultrasonic P-wave velocities in 132 directions at the reservoir pressure. After transforming the data to the symmetry axis coordinates, we find Thomsen's anisotropy parameters δ and ɛ using these measurements and measurements of the shear-wave velocity along the symmetry axis from a well log. To find these anisotropy parameters, we use a very fast simulated re-annealing algorithm with an objective function that contains only the measured ray velocities, their numerical derivatives and the unknown elasticity parameters. The results show strong elliptical anisotropy in the overburden shale. This approach produces smaller uncertainty of Thomsen parameter δ than more direct approaches.

dc.publisherWiley-Blackwell Publishing Ltd.
dc.subjectAnnealing
dc.subjectAzimuth
dc.subjectSpherical
dc.titleThomsen's parameters from p-wave measurements in a spherical sample
dc.typeJournal Article
dcterms.source.issn0016-8025
dcterms.source.titleGeophysical Prospecting
curtin.note

First published online: August 17, 2010

curtin.departmentDepartment of Exploration Geophysics
curtin.accessStatusFulltext not available


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