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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
1

Aeromagnetic interpretation of a section of the Willyama Inliers in the Curnamona Craton, South Australia / Mohammad Reza Haidarian.

Haidarian, Mohammad Reza January 1996 (has links)
Figure 5.13 is folded and in plastic pocket inside back cover. / Bibliography: leaves 147-168. / xiv, 184, [14] leaves, [35] leaves of plates : ill. (chiefly col.), maps ; 30 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1998
2

Interpretation of aeromagnetic data of the Olary province, South Australia and the development of interpretation methods / by Nnaemeka Francis Ukaigwe

Ukaigwe, Nnaemeka Francis January 1985 (has links)
6 folded (5 of them maps) in pocket / Includes bibliography / xvii, 102, 8, 5, 10 [i.e. ca. 500] leaves (some folded) : ill., maps (some col.) ; 30 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1985
3

Developing a tectonic framework for the Southern Curnamona Cu - Au Province : geochemical and radiogenic isotope applications

Rutherford, Lachlan Stuart January 2006 (has links)
"Two independent geochronological techniques specifically targeting post-kinematic or late-stage growth of kyanite, staurolite and late-stage garnet in the southern Curnamona Province has found that these minerals grew during the Delamerian Orogeny (~530-500 Ma). Prograde metamorphism during the Delamerian Orogeny attained kyanite-staurolite-garnet grade (amphibolite-facies). Previous interpretations of an anticlockwise P-T path for the Olarian Orogeny need revising, as these interpretations have been shown in this study to be based on textural relationships spanning ~1100 million years. This highlights the importance of in situ geochronological techniques in defining robust P-T-t paths for a region." --p. 121 of source document. / Thesis (Ph.D.)--School of Earth and Environmental Sciences, 2006.

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