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Статті в журналах з теми "Willyama Supergroup"
Stevens, B. P. J., and G. M. Bradley. "Sedimentology in metamorphic rocks, the Willyama Supergroup, Broken Hill, Australia." Australian Journal of Earth Sciences 65, no. 1 (December 3, 2017): 25–59. http://dx.doi.org/10.1080/08120099.2018.1399462.
Повний текст джерелаStevens, B. P. J., and G. J. Corbett. "The Redan Geophysical Zone: Part of the Willyama Supergroup? Broken Hill, Australia." Australian Journal of Earth Sciences 40, no. 4 (August 1993): 319–38. http://dx.doi.org/10.1080/08120099308728084.
Повний текст джерелаStevens, B. P. J., R. W. Page, and A. Crooks‡. "Geochronology of Willyama Supergroup metavolcanics, metasediments and contemporaneous intrusions, Broken Hill, Australia." Australian Journal of Earth Sciences 55, no. 3 (April 2008): 301–30. http://dx.doi.org/10.1080/08120090701769456.
Повний текст джерелаSTEVENS, B., R. BARNES, R. BROWN, W. STROUD, and I. WILLIS. "The Willyama Supergroup in the Broken Hill and Euriowie Blocks, New South Wales." Precambrian Research 40-41 (October 1988): 297–327. http://dx.doi.org/10.1016/0301-9268(88)90073-3.
Повний текст джерелаStevens, B. P. J. "Post‐depositional history of the Willyama Supergroup in the Broken Hill Block, NSW." Australian Journal of Earth Sciences 33, no. 1 (March 1986): 73–98. http://dx.doi.org/10.1080/08120098608729351.
Повний текст джерелаBodorkos, S., and J. A. Fitzherbert. "Timing and significance of pre-Olarian metamorphism in the Willyama Supergroup, Broken Hill, Australia." Precambrian Research 378 (August 2022): 106772. http://dx.doi.org/10.1016/j.precamres.2022.106772.
Повний текст джерелаPepper, M. A., and P. M. Ashley. "Volcanic textures in quartzo‐feldspathic gneiss of the Willyama Supergroup, Olary Domain, South Australia." Australian Journal of Earth Sciences 45, no. 6 (December 1998): 971–78. http://dx.doi.org/10.1080/08120099808728451.
Повний текст джерелаKent, A. J. R., P. M. Ashley, and C. M. Fanning. "Metasomatic alteration associated with regional metamorphism: an example from the Willyama Supergroup, South Australia." Lithos 54, no. 1-2 (October 2000): 33–62. http://dx.doi.org/10.1016/s0024-4937(00)00021-9.
Повний текст джерелаAshley, P. M., B. G. Lottermoser, and J. M. Westaway. "Iron-formations and epigenetic ironstones in the Palaeoproterozoic Willyama Supergroup, Olary Domain, South Australia." Mineralogy and Petrology 64, no. 1-4 (March 1998): 187–218. http://dx.doi.org/10.1007/bf01226569.
Повний текст джерелаBierlein, F. P., U. Haack, B. Förster, and I. R. Plimer. "Lead isotope study on hydrothermal sulfide mineralisation in the Willyama Supergroup, Olary Block, South Australia." Australian Journal of Earth Sciences 43, no. 2 (April 1996): 177–87. http://dx.doi.org/10.1080/08120099608728246.
Повний текст джерелаДисертації з теми "Willyama Supergroup"
Bradbury, Georgina A. "The structural and mineralogical features of the Willyama Supergroup, near Mutooroo Homestead, Olary Block, South Australia /." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bb798.pdf.
Повний текст джерелаLeah, Peter A. "Petrology, structure and stratigraphy of the Willyama Supergroup and Olarian granitoids, west of Plumbago Homestead, Olary Block, South Australia /." Title page, contents and abstract only, 1985. http://web4.library.adelaide.edu.au/theses/09SB/09sbl435.pdf.
Повний текст джерелаTaylor, A. D. "Structural mapping adjacent to the “Woman-in-White” amphibolite in the Olary Domain, South Australia." Thesis, 1999. http://hdl.handle.net/2440/119337.
Повний текст джерелаA structural study of Palaeoproterozoic Willyama Supergroup rocks to the southeast of Old Boolcoomata approximately 20 kilometres north of Olary, South Australia, discloses a complex history of deformation. This includes an axial planar S1 schistosity and several intersecting locally developed subsequent planar fabrics. The main findings support previous unpublished company studies. Structural maps were produced at various scales in areas surrounding the ‘Woman-in-White’ amphibolite and all available observations were used to form a chronology of events and tectonic model for the geometric and kinematic evolution of the area. In a domain east of the 'Woman-in-White' amphibolite the S1 is parallel to the axial plane of a major isoclinal synform closing to the east. S2 is axial planar to tight to open class 2 and class 1c F2 folds that trend generally north to northeast. Regionally, and particularly in the vicinity of the 'Woman-in-White' amphibolite, a third deformation is very intensely developed generating two fabrics. The S3 schistosity is the axial planar fabric to tight to isoclinal F3 folds trending consistently east-west. The S3 fabric is also expressed as a crenulation of the S1 regional schistosity. These pre-Adelaidean structural elements are recognised as comprising the Olarian Deformation. Fold interference is present on all scales. Olarian deformation events two and three have given the flat lying western limb of the principal F1 synform a luniform, dome and basin morphology. Type 2 and type 3 interference patterns are the most common in the area mapped. The occurrence of the two interference patterns is due to the variable angle between OD2 and OD3 compressions, which is commonly approximately 40 in the west-southwest part of the mapped area. This work conforms closely in complexity to previous regional studies and has been supplemented by other new investigations of an important northeast-southwest trending shear zone corresponding to OD3, lying further to the north, and a geochemical investigation of the 'Woman-in-White' amphibolite indicating its probable mantle origin and possible emplacement before all deformations occurred.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1999