Добірка наукової літератури з теми "Arkaroola"
Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями
Ознайомтеся зі списками актуальних статей, книг, дисертацій, тез та інших наукових джерел на тему "Arkaroola".
Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.
Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.
Статті в журналах з теми "Arkaroola"
KALLIES, AXEL, and TED EDWARDS. "A new sun moth species from the Flinders Ranges in South Australia (Lepidoptera, Castniidae)." Zootaxa 4369, no. 2 (January 3, 2018): 292. http://dx.doi.org/10.11646/zootaxa.4369.2.9.
Повний текст джерелаBons, Paul. "Photograph of the Month: Antitaxial fibrous calcite vein, Arkaroola, South Australia." Journal of Structural Geology 31, no. 7 (July 2009): 627. http://dx.doi.org/10.1016/j.jsg.2008.10.019.
Повний текст джерелаCollier, J. B., and I. R. Plimer. "Supergene clinobisvanite pseudomorphs after supergene dreyerite from Lively's Mine, Arkaroola, South Australia." Neues Jahrbuch für Mineralogie - Monatshefte 2002, no. 9 (September 24, 2002): 401–10. http://dx.doi.org/10.1127/0028-3649/2002/2002-0401.
Повний текст джерелаLaing, Jennifer H., J. Clarke, J. Deckert, V. Gostin, J. Hoogland, L. Lemke, J. Leyden, et al. "Using an Australian Mars Analogue Research Facility for Astrobiology, Education and Outreach." Symposium - International Astronomical Union 213 (2004): 553–58. http://dx.doi.org/10.1017/s0074180900193891.
Повний текст джерелаWood, P. R., A. W. Rodgers, and K. S. Russell. "Seeing Measurements at Freeling Heights and Siding Spring Observatory." Publications of the Astronomical Society of Australia 12, no. 1 (April 1995): 97–105. http://dx.doi.org/10.1017/s1323358000020129.
Повний текст джерелаBons, Paul D., Michael Montenari, Ronald J. Bakker, and Marlina A. Elburg. "Potential evidence of fossilised Neoproterozoic deep life: SEM observations on calcite veins from Oppaminda Creek, Arkaroola, South Australia." International Journal of Earth Sciences 98, no. 2 (October 5, 2007): 327–43. http://dx.doi.org/10.1007/s00531-007-0245-4.
Повний текст джерелаBakker, Ronald J., and Marlina A. Elburg. "A magmatic-hydrothermal transition in Arkaroola (northern Flinders Ranges, South Australia): from diopside–titanite pegmatites to hematite–quartz growth." Contributions to Mineralogy and Petrology 152, no. 5 (August 1, 2006): 541–69. http://dx.doi.org/10.1007/s00410-006-0125-0.
Повний текст джерелаWawryk, A. "Conservation and Access to Land for Mining in Protected Areas: The Conflict Over Mining in South Australia's Arkaroola Wilderness Sanctuary." Journal of Environmental Law 26, no. 2 (May 19, 2014): 291–317. http://dx.doi.org/10.1093/jel/equ008.
Повний текст джерелаColyer, Kate, Jamie S. Quinton, Allan Pring, Rachel S. Popelka-Filcoff, and Claire E. Lenehan. "Determining the origins of particulates on Arkaroo Rock art." Open Journal of Archaeometry 2, no. 1 (February 12, 2014). http://dx.doi.org/10.4081/arc.2014.5301.
Повний текст джерелаДисертації з теми "Arkaroola"
Hansberry, R. L. "Tectonic evolution of the Arkaroola Basin: implications for the development of the Adelaide Rift Complex." Thesis, 2011. http://hdl.handle.net/2440/96126.
Повний текст джерелаThe Neoproterozoic to Cambro-Ordovician sediments of the Adelaide Rift Complex (formerly Adelaide Geosyncline) have been the focus of extensive investigation. Despite this, comparatively little is known about the Earliest Adelaidean Callanna Group sediments, due to their sparse preservation in outcrop geology. Exposure of the Callanna Group, and structures related to early Cryogenian graben formation at Arkaroola, in the northern Flinders Ranges, provides a unique opportunity to unravel the local geometries of rift initiation. These rocks have been subjected to multiple intracontinental deformations, most notably the Delamerian Orogeny. Through detailed structural mapping and analysis it is possible to propose models of tectonic evolution for this area. Previous regional scale mapping of the northern Flinders Ranges has identified a disparity between the tectonic history of the Arkaroola Basin and broader northern Flinders Ranges. The nature of the rifting and orogenic evolution of the Arkaroola Basin is determined though analysis of field data, rock samples in thin section and EBSD analysis. Graben formation accommodated an initial period of clastic and evaporitic deposition, followed by rift related basalt extrusion. This was followed by several phases of localised rifting and deposition, controlled by evolving fault geometries. Broad-scale orthogonal folding has folded an earlier composite fabric in conjunction with bedding. This initially planar fabric, most notable in the Woodnamoka Phyllite, formed during peak metamorphism of at least 500° C and approximately 3 kbars and is primarily attributed to burial beneath a thick pile of rift and sag phase sediments, coupled with a change in horizontal stresses. This is loosely constrained to post-rift cessation and before a previously indentified thermal pulse, ca 440 Ma. A set of NE-SW trending faults in the basin have been identified as En echelon stepovers of the Paralana Fault system, responsible for the formation of the pull-apart geometries. This system of faults details a strike-slip duplex, the reactivation of which, coupled with an anomalously high-heat producing basement, has controlled and localised deformation of the Arkaroola Basin.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Prohoroff, A. "Structural and Metamorphic Conditions of the Lower Burra Group and Callana Group at Arkaroola, Northern Flinders Ranges." Thesis, 2013. http://hdl.handle.net/2440/106297.
Повний текст джерелаThe lowermost Adelaidean sequences exposed to the immediate north of Arkaroola are unusual as they exhibit a localised complexity of deformation and elevated metamorphic grade that is not observed elsewhere in the Adelaide Fold Belt. Deformation and metamorphism in Arkaroola is thought to have formed as part of the Delamerian Orogen approximately 515-490 Ma. The timing of deformation and metamorphism however is poorly constrained in this area. This paper aims to discuss the structural and metamorphic conditions in the area to determine if there was a possibility of a pre or post-Delamerian structural and/or thermal event. A section was mapped to the North-East of the Arkaroola Homestead to gain an insight into the structural and metamorphic conditions of the area. Samples were collected from the field and used for microstructural analysis. An Electron Microprobe, Laser Ablation Inductively Coupled Plasma Mass Spectrometer and an XRF spectrometer were used for geochemical analysis on the samples. Structural and stratigraphic observations combined with microstructural analysis of samples from the field helped the author create an interpreted geological history of the area. Graben formation accommodated an initial period of sediment deposition followed by basalt extrusion. Several phases of localised rifting and deposition followed this initial deposition period due to changing fault geometries. A mineral fabric that occurs parallel to bedding is seen throughout the study area. This fabric is overgrown and included in prominent cordierite porphyroblasts that formed during peak metamorphism of ≥500 °C at a pressure of approximately ~1.30kbars. These pressure and temperature conditions were primarily due to the burial beneath a thick cover of sediments. A number of faults trending in a NE-SW direction have been identified as splays from the Paralana fault system. The strike-slip movement of the Paralana Fault along with the high heat producing basement of the Mount Painter Inlier has controlled the localised structural complexity and elevated metamorphic grade in the Arkaroola area.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2013
Berthiaume, Jonathan David Donauer. "Neotectonic faults of the Paralana Escarpment and their influence on uranium-bearing fluid flow." Thesis, 2018. http://hdl.handle.net/2440/118205.
Повний текст джерелаThesis (MPhil) -- University of Adelaide, School of Physical Sciences, 2018
Morphett, W. J. "Geochronological and structural insights into the evolution of the Lower Burra and Callana Groups near Arkaroola: structural mapping and U-Pb metamorphic monazite dating." Thesis, 2013. http://hdl.handle.net/2440/106291.
Повний текст джерелаThe lowermost sediments of the Adelaide Supergroup near Arkaroola display pronounced structural complexity and anomalously high metamorphic grade. The timing of the structures, fabrics and metamorphism in the region remain unconstrained, although all are currently interpreted to have occurred during the Delamerian Orogeny. Monazite U/Pb geochronology provides a useful technique for dating amphibolites facies rocks and, combined with map scale and micro structural observations, suggests the peak metamorphism and at least one deformation event occurred significantly earlier than the Delamerian Orogeny. Monazite derived 206Pb/238U age estimates place the timing of peak metamorphism at 705.2±7.4 Ma with observations from thin section revealing a bedding parallel fabric pre-dating peak metamorphism. U/Pb analysis also reveals a second monazite growth event at 644.2±8 Ma the cause of which is hypothesised to be fluid related. Regional folding and axial planar fabric generation post-dates this metamorphism and can be seen to overprint the earlier fabric and wrap the cordierite porphyroblasts. This final deformation event remains largely unconstrained as in situ dating of monazite was not possible in this study. The inferred parasitic relationship between the folds within the studied region and the Arkaroola Syncline which folds the youngest sediments in the Adelaidian Sequence allows for the deposition to be constrained subsequent to the conclusion of the Adelaide Rift Complex.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2013
Job, A. L. "Evolution of the basal Adelaidean in the northern Flinders Ranges: deposition, provenance and deformation of the Callanna and lower Burra Groups." Thesis, 2011. http://hdl.handle.net/2440/96175.
Повний текст джерелаThe rift and deformational evolution of the Adelaide Fold Belt’s northern-most extent, the northern Flinders Ranges, has received comparatively little attention than that of the southern Adelaide Fold Belt. The Arkaroola area, located in the mid-north northern Flinders Ranges, exposes the lowermost Adelaidean stratigraphy of this rift complex, the Callanna and lower Burra Groups, in a near complete sedimentary sequence. The rift history of this stratigraphy is complex, with deposition being largely controlled by the northeast-southwest orientated Paralana Fault and similarly orientated local growth faults. Locally, the Paralana Fault deviates from its regional orientation and forms a north-south striking segment, which under a considered sinistral strike-slip regime during extension would potentially create localised transtension in a ‘releasing bend’ environment. Rifting in the Arkaroola area is therefore considered to be analogous to the formation of a pull-apart basin. U-Pb dating of detrital zircons from the Paralana Quartzite, Humanity Seat Formation and Blue Mine Conglomerate from the Callanna and lower Burra groups yields ages that are comparable to local source regions the Gawler Craton, Mount Painter Basement Complex and the Curnamona Province, and suggest proximal derivation during early rift phases. Sm-Nd bulk rock analysis on the finer grained Woodnamoka Formation implies derivation from the Mount Painter Basement Complex or the upper Willyama Supergroup of the Curnamona Province, the latter of which potentially suggests a more distal provenance region outside of the Australian continent. Deformation in the northern Flinders Ranges has previously been largely ascribed to the ca. 500 Ma Delamerian Orogeny. However, the Arkaroola area exhibits complex deformation not observed in the directly overlying gently folded stratigraphy. Reactivation of pull-apart rift structures during transpression is considered a possible mechanism for producing and localising such deformation. The possibility of an early Neoproterozoic deformational event occurring prior to deposition of the lesser-deformed overlying stratigraphy is also considered, but in lieu of an unequivocal orogenic unconformity, cannot be confidently ascribed. Temporal constraints defined by this study are too broad to accurately define the timing of deformation, and therefore its timing and potential relationship to the Delamerian Orogeny remains largely enigmatic.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Книги з теми "Arkaroola"
Rock star: The story of Reg Sprigg - an outback legend. Hindmarsh, S. Aust: East Street Publications, 2008.
Знайти повний текст джерела(Photographer), Pete Dobre', ed. Arkaroola: Northern Flinders Ranges, South Australia. Oz Scapes, 2000.
Знайти повний текст джерелаТези доповідей конференцій з теми "Arkaroola"
Champenois, France, Annette George, and Maree Corkeron. "Filamentous cyanobacteria in reefal facies of the Neoproterozoic Arkaroola reef complex, Flinders Ranges, South Australia." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11695.
Повний текст джерела