Dissertationen zum Thema „Paleobiology South Australia Fleurieu Peninsula“
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Bickford, Sophia Anastasia. „A historical perspective on recent landscape transformation: integrating palaeoecological, documentary and contemporary evidence for former vegetation patterns and dynamics in the Fleurieu Peninsula, South Australia“. Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09PH/09phb583.pdf.
West, Andrew S. „The shore platforms of the Fleurieu Peninsula, South Australia /“. Title page, abstract and table of contents only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbw516.pdf.
Collings, Greg. „Spatiotemporal variation of macroalgal communities of southern Fleurieu Peninsula, South Australia /“. Title page, table of contents and summary only, 1996. http://web4.library.adelaide.edu.au/theses/09PH/09phc711.pdf.
Boord, R. A. „Sedimentology of the Cambrian, Upper Kanmantoo Group, Southern Fleurieu Peninsula, South Australia /“. Title page, contents and abstract only, 1985. http://web4.library.adelaide.edu.au/theses/09AR/09arb724.pdf.
Stolz, Ned. „A magnetics study of the Brachina Formation on southern Fleurieu Peninsula, South Australia /“. Adelaide, 1985. http://web4.library.adelaide.edu.au/theses/09SB/09sbs876.pdf.
Szmidel, Rebekah. „The structural geology of Sellick Hill to Myponga Beach, Fleurieu Peninsula, South Australia /“. Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbs998.pdf.
National Grid reference (SI-54)6527 - II, (SI-54) 6627 - III 1:10 000 sheet. Includes bibliographical references (leaves 32-39).
Crowhurst, Peter V. „The geology, petrology and geochemistry of the Proterozoic Inlier, south of Myponga, Fleurieu Peninsula, South Australia /“. Title page, contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09SB/09sbc953.pdf.
Barrett, Lyon. „The structural geology of the Rapid Bay-Second Valley area, Fleurieu Peninsula, South Australia /“. Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbb274.pdf.
Macdonald, Andrew. „The structural geology of the Yohoe Creek to Cape Jervis area, Fleurieu Peninsula, South Australia /“. Title page, contents and introduction only, 1995. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bm1348.pdf.
Kapetas, John. „The structure of the Clarendon - Mt. Bold region : southern Adelaide fold belt, Fleurieu Peninsula, South Australia /“. Title page, abstract and contents only, 1993. http://web4.library.adelaide.edu.au/theses/09SB/09sbk17.pdf.
Buhrer, Daniel Anton. „The structure of Myponga River-Carrickalinga Creek area, Southern Adelaide Fold Belt, Fleurieu Peninsula, South Australia /“. Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbb931.pdf.
National Grid reference (SI 54) 6527-36 ; 44, 45, 36, 37 1:10 000 sheets. Includes bibliographical references.
Harvey, Leslie M. „Examination of an aeromagnetic anomaly over the Talisker Mine area on the southern Fleurieu Peninsula, South Australia /“. Title page, contents and abstract only, 1989. http://web4.library.adelaide.edu.au/theses/09SB/09sbh342.pdf.
Bickford, Sophia Anastasia. „A historical perspective on recent landscape transformation: integrating palaeoecological, documentary and contemporary evidence for former vegetation patterns and dynamics in the Fleurieu Peninsula, South Australia / Sophia Anastasia Bickford“. Thesis, 2001. http://hdl.handle.net/2440/21741.
xx, 319, [30] leaves : ill. (some col.), maps ; 30 cm.
Palaeoecological records, documented historical records and remnant vegetation were investigated in order to construct a multi-scaled history of vegetation pattern and change in the Fleurieu Peninsula, South Australia over the last c. 8000 years. Aims to better understand post-European landscape transformation and address the inherently historical components of the problems of regional biodiversity loss, land sustainability and the cumulative contribution to global climatic change.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geographical and Environmental Studies, 2001
Collings, Gregory James. „Spatiotemporal variation of macroalgal communities of southern Fleurieu Peninsula, South Australia / by Gregory James Collings“. 1996. http://hdl.handle.net/2440/18910.
2 v. : ill. (some col.), maps ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
The temporal dynamics of eight subtidal mixed macroalgal communities were quantified. The results were discussed in terms of the implications for sampling programs in the future and the reliability of previous work.
Thesis (Ph.D.)--University of Adelaide, Dept. of Botany, 1997?
Collings, Gregory James. „Spatiotemporal variation of macroalgal communities of southern Fleurieu Peninsula, South Australia / by Gregory James Collings“. Thesis, 1996. http://hdl.handle.net/2440/18910.
2 v. : ill. (some col.), maps ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
The temporal dynamics of eight subtidal mixed macroalgal communities were quantified. The results were discussed in terms of the implications for sampling programs in the future and the reliability of previous work.
Thesis (Ph.D.)--University of Adelaide, Dept. of Botany, 1997?
Barrett, L. „The structural geology of the Rapid BaySecond Valley area, Fleurieu Peninsula, South Australia“. Thesis, 1995. http://hdl.handle.net/2440/128629.
Whilst the geology of the Rapid Bay-Second Valley area is known to be both structurally and stratigraphically complex, previous workers (Daily, 1963; Evans 1987; Drayton, 1963; Campana and Wilson, 1955) have been unable to agree on many aspects of the area. Neoproterozoic and Cambrian aged sediments were first deposited in an extensional basin, which was formed due to lithospheric thinning, and associated subsidence (Jenkins, 1986, 1990). These rocks have then been subjected to at least one phase of deformation, the Cambro-Ordovician Delamerian Orogeny (Offler & Fleming, 1968; Thompson, 1970). Listric extensional faults were formed both before and during sedimentation of the rocks, which has created narrow zones of weakness that the subsequent compressional event has exploited, creating thrust faults (Flottman et al., 1994). Structural mapping of the area has revealed that it is transected by two thrust faults and is intensely folded in places. Structural data has been collected during eight weeks of field work and has been compiled into a 1:10 000-scale geological map which accurately represents the area. A computer-generated three-dimensional model has been created for the area, based on this map, and cross and profile sections constructed from the data collected. The model was constructed using Vulcan™ software. Strain analysis has also been conducted on many of the folds in the area.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1995
Crowhurst, P. V. „The geology, petrology and geochemistry of the Proterozoic inlier, south of Myponga, Fleurieu Peninsula, South Australia“. Thesis, 1988. http://hdl.handle.net/2440/119710.
The study area is located within the Yankalilla-Myponga Proterozoic lnlier, approximately 60km south of Adelaide. The basement rocks are comprised of a mixture of metasediments and intrusives. The metasediments predominantly comprise of quartz-biotite gneisses and schists. They are intruded by basic dykes, pegmatites and an aplite/microgranite. The basic dykes have oceanic basalt affinities and could originally have been formed during an 'aborted rifting' event, but the more felsic rocks are more likely to lie within plate granites. The origin of the 'Houghton' granulite is difficult to ascertain, because it has a varied internal composition and is closely comparable to a diorite and a shale. The basement inlier rocks are found within the overlying unconformable upper Proterozoic Adelaidean System. They have undergone at least four phases of deformation and metamorphism. Mineral assemblages found in the rocks indicate metamorphism reached at least upper amphibolite facies. The maximum pressure and temperature conditions were calculated from microprobe data. They range from 8-10 kb at 550 -650 C. U-Pb isochron dating was performed on the aplite/microgranite of the area and was found to be 1578+\-22Ma ,which places a minimum age on the inlier rocks. This date obtained and the deformation processes recognized are comparable to other basement rocks in South Australia; noticeably the Gaw1er Craton and the Olary Province. This may indicate a homogeneous terrain once spanned most of South Australia during the lower Proterozoic.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1988
Harvey, L. M. „Examination of an aeromagnetic anomaly over the Talisker Mine area on the southern Fleurieu Peninsula, South Australia“. Thesis, 1989. http://hdl.handle.net/2440/119293.
A N-E striking elongate aeromagnetic anomaly is observed over the Talisker Mine area, on the southern Fleurieu Peninsula, which has character and amplitude similar to an anomaly observed at Delamere (several kilometres to the north) found to be caused by magnetic Brachina Formation. Geological and geophysical techniques have been used to determine if the rock type at Talisker is also magnetic Brachina Formation, why there is a gap between the two anomalies, and why the anomaly at Talisker ends near the south coast. Geological mapping, microscopy and petrologic studies have been used in conjunction with local ground magnetic surveys and modelling procedures, to reveal magnetic Brachina Formation as the cause of the anomaly at Talisker. Mapping has shown the anomaly to be the result of a sliver of magnetic Brachina Formation caught up within a local zone of intense deformation that extends for at least 1500m across strike, and which outcrops on the coast. The Brachina Formation is sheared out against Cambrian Backstairs Passage Formation to the south, forming the southern end to the anomaly. To the north, the Brachina Formation suffered deeper erosion during Permian times, and is covered by a greater thickness of non-magnetic cover which causes the apparent gap in the aeromagnetic anomaly.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1989