Tertiary uplift and its implications for the tectonic evolution of sedimentary basins, offshore south-west United Kingdom / Robert John Menpes.

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dc.contributor.authorMenpes, Roberten
dc.contributor.schoolDept. of Geology and Geophysicsen
dc.date.issued1997en
dc.descriptionCopies of author's previously published works inserted.en
dc.descriptionBibliography: p. 157-165.en
dc.descriptionix, 165 p. : ill. (chiefly col.), maps ; 30 cm.en
dc.description.abstractSonic velocities from the Danian Chalk, Upper Cretaceous Chalk, Lower Cretaceous Greensand/Gault Clay, Lower Cretaceous Wealden, Upper Jurassic mudstones, Triassic Mercia Mudstone, and Triassic Sherwood Sandstone have been used to quantify apparent exhumation in the Celtic Sea/South Western Approaches.en
dc.description.dissertationThesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1998en
dc.format.extent341531 bytesen
dc.format.mimetypeapplication/pdfen
dc.identifier.urihttp://hdl.handle.net/2440/19194
dc.language.isoenen
dc.provenanceThis electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exception. If you are the author of this thesis and do not wish it to be made publicly available or If you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legals. Copyright material removed from digital thesis. See print copy in University of Adelaide Library for full text.en
dc.subject.ddc551.8/09/41 21en
dc.subject.lcshSedimentary structures Great Britain.en
dc.subject.lcshGeology, Structural Great Britain.en
dc.titleTertiary uplift and its implications for the tectonic evolution of sedimentary basins, offshore south-west United Kingdom / Robert John Menpes.en
dc.typeThesisen

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