Academic literature on the topic 'Warumpi Province'
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Journal articles on the topic "Warumpi Province"
Kultys, Kamil, Kamil Misztal, and Maria Stadnicka. "Wykorzystanie energii wiatru i wody do celów gospodarczych w XIX i XX wieku w zlewni Zagożdżonki." Prace Geograficzne, no. 167 (October 31, 2022): 69–89. http://dx.doi.org/10.4467/20833113pg.22.008.16221.
Full textAdeney, Frances. "Why Biography? Contributions of Narrative Studies to Mission Theology and Mission Theory Contribution des études narratives à la théologie et à la théorie de la mission Warum Biografie? Beiträge von narrativen Studien zur Missionstheologie und Missionstheorie Biografía, por y para qué. Contribuciones del estudio de casos a la teología y a la teoría de la misión." Mission Studies 26, no. 2 (2009): 153–72. http://dx.doi.org/10.1163/016897809x12548912398758.
Full textWARUI, MARY WANJIRU, SHYAM MANOHAR, and PAUL OBADE. "Current status, utilization, succession and zonation of mangrove ecosystem along Mida Creek, Kenya." International Journal of Bonorowo Wetlands 10, no. 1 (February 14, 2020). http://dx.doi.org/10.13057/bonorowo/w100103.
Full textDissertations / Theses on the topic "Warumpi Province"
Trestrail, J. L. "U-Pb detrital zircon, geochemical and Nd isotope constraints on sedimentary provenance of the Chewings Range Quartzite, Warumpi Province, Arunta Region, NT." Thesis, 2010. http://hdl.handle.net/2440/106279.
Full textThe Chewings Range Quartzite is a meta-sedimentary cover sequence located in the Warumpi Province of the Arunta Region. U-Pb detrital Zircon analysis of the Chewings Range Quartzite indicates a minimum depositional age of ~ 1640Ma, with the main population of zircons residing within a range of 1700 – 1800Ma. Evidence from Sm-Nd isotopic data suggests that a series of Staurolite Garnet Schists, often grouped with the Chewings Range Quartzite, has a significantly more juvenile character. This suggests that it may represent a new unit with a significantly differing provenance to that of the Chewings Range Quartzite. Combined REE, geochemistry and detrital zircon dating suggests that the Chewings Range Quartzite was derived primarily off the Arunta Region and North Australian Craton, while the Stauralite Garnet Schists holds more affinity with juvenile Musgrave Province to the south.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Fields, C. E. "Liebig-aged (c. 1640 Ma) magmatism and metamorphism in c. 1760 Ma crust in the Warumpi and southern Aileron Province, central Australia: a case for revising the tectonic framework of Proterozoic Australia." Thesis, 2012. http://hdl.handle.net/2440/92217.
Full textThe southern margin of the North Australian Craton (NAC) has been suggested to represent a long-lived (c. 1860 to 1600 Ma) active margin that preserves a cryptic record of the growth and assembly of the Australian continent. The Warumpi Province is juxtaposed against the southern Aileron Province, and has been interpreted as exotic to the NAC, though the timing of collision between the Warumpi Province and the southern Aileron Province is contentious. U-Pb zircon and monazite LA-ICP-MS geochronology from granulite facies metapelites and granitic gneisses along the southern margin of the Aileron Province and northern margin of the Warumpi Province, has shown it is characterised by c. 1780-1740 Ma magmatic rocks and c. 1640-1615 Ma magmatic and metamorphic rocks. The evidence for these events is preserved in kilometre-scale migmatitic boudins and low-strain zones enveloped by pervasive E-W trending higher strain belts. The overprinting high strain fabrics are Grenvillian age and constrained to c. 1175-1070 Ma. Phase equilibria modelling on a garnet-sillimanite-cordierite metapelite dated at c.1616 Ma, from a low-strain domain within the southern Aileron Province, indicates that peak metamorphic conditions were ~7-8 kbar and between 740-900 °C, and were associated with a down-pressure or decompressional P-T history. A metamorphic monazite age of c.1620 Ma was also preserved in a granitic gneiss located in an older, low-strain domain. The presence of the c. 1760 Ma and c. 1640 Ma timelines in both the Warumpi and Aileron Provinces calls into question the proposed exotic nature of the Warumpi Province. A speculative interpretation is that the Liebig-aged metamorphism and magmatism, seemingly associated with relatively shallow orientated, low strain fabrics, represents a period of extension rather than collision.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2012
Greenslade, M. M. "Ultrahigh temperature metamorphism: testing models for collision vs extension." Thesis, 2015. http://hdl.handle.net/2440/118029.
Full textThe Warumpi Province has been interpreted to be exotic and accreted to the Northern Australian Craton (NAC) during the Liebig Orogeny at c.1640Ma. However, phase equilibria modelling of melt-deficient, Mg-Al rich granulite facies rocks at Hill 830, in the Mount Liebig area show contradictory evidence of a decompressional pressure-temperature path and a high metamorphic gradient of 90°Ckbar. This interpretation in conjunction with abundant c.1780- 1740Ma and c.1640Ma magmatism in the southern Aileron and Warumpi Provinces, indicate that the tectonic regime at c.1640Ma may instead be a south-migrating, extensional scenario, compared to the previously accepted collisonal regime; speculating that the Warumpi Province is not ‘exotic’ to the NAC.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2015
Oertel, A. G. "Magnetotelluric survey of the Central Australian Craton, with a focus on the structural history of the Warumpi and Musgrave Provinces and the Arunta Complex." Thesis, 2013. http://hdl.handle.net/2440/106295.
Full textIn spite of the continent of Australia being the oldest and most tectonically stable on Earth, its structural history is still the subject of much conjecture. The final closure of the South Australian Craton with the North Australian Craton at roughly 1080 million years ago deformed much of Central Australia into the lithospheric arrangement observed today. Structural constraints have been developed in the last 30 years on the history of the Musgrave Province, Amadeus Basin, Warumpi Province and Arunta Complex in the southern part of the Northern Territory. In this study the resistivity structure of these four provinces was assessed through the use of a long-period magnetotelluric survey along the Stuart Highway from the South Australia-Northern Territory border to 90 kilometres north of Alice Springs. A key focus was to determine whether the structural arrangement, identified in a magnetotelluric survey conducted 100 kilometres to the east of this profile in 2006, is laterally consistent between the four provinces. In the Stuart Highway profile model the major structures present exhibit a different arrangement, particularly in the northern part of the profile, resulting in the conclusion that the mechanism for the lithospheric closure of the region was a more complex nature than was previously thought.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2013
Book chapters on the topic "Warumpi Province"
"5. Kärnten – oder: Warum ein Toter Wahlen gewinnt (und seine Erben alles verlieren)." In Erdbeben in der Provinz, 155–220. Wien: Böhlau Verlag, 2013. http://dx.doi.org/10.7767/boehlau.9783205789680.155.
Full textMaier, Andreas. "Provinz, Dorf, Heimat oder Warum ich neuerdings so oft eingeladen werde." In Gutes Leben auf dem Land?, 239–52. transcript Verlag, 2021. http://dx.doi.org/10.1515/9783839454251-007.
Full textConference papers on the topic "Warumpi Province"
March, Samantha, Martin Hand, Laura Morrissey, and David Kelsey. "Enigmatic ultrahigh-temperature metamorphism in the Warumpi Province: Continental collision or extension?" In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11742.
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