Academic literature on the topic 'Mt Boothby'
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Journal articles on the topic "Mt Boothby"
Lancaster, Ron, and Jim Sandefur. "Mathematical Lens: Boothbay Harbor, Maine." Mathematics Teacher 98, no. 3 (October 2004): 164–65. http://dx.doi.org/10.5951/mt.98.3.0164.
Full textSmith, H. Clay. "Reconsidering the Composition of Ezra-Nehemiah in Light of 2 Maccabees 1:10–2:18." Journal of Biblical Literature 141, no. 2 (June 15, 2022): 257–76. http://dx.doi.org/10.15699/jbl.1412.2022.4.
Full textMcLoughlin, John Grant. "Solutions to Calendar." Mathematics Teacher 90, no. 3 (March 1997): 218–19. http://dx.doi.org/10.5951/mt.90.3.0218.
Full textFitriana, Mira, Suzanna Ratih Sari, and Siti Rukayah. "FAKTOR – FAKTOR PENGARUH PREFERENSI PENGGUNA PASAR PETEROGAN SEMARANG PASCA REVITALISASI." Jurnal Arsitektur ARCADE 4, no. 1 (March 20, 2020): 65. http://dx.doi.org/10.31848/arcade.v4i1.328.
Full text"MSA MegaBooth." Microscopy and Microanalysis 15, S1 (June 5, 2009): 18. http://dx.doi.org/10.1017/s1431927609090461.
Full textDissertations / Theses on the topic "Mt Boothby"
Howlett, D. P. "Geochronological constraints on Yambah and Chewings-aged deformation at Mt Boothby in the south eastern Reynolds Range, Central Australia." Thesis, 2012. http://hdl.handle.net/2440/92257.
Full textZircon and monazite U–Pb isotope geochronology combined with structural mapping in the Mt Boothby region in the central Aileron Province in Central Australia has constrained the timing of two tectonically distinct phases of high-grade deformation and metamorphism. The first event (D1/M1) occurred at around 1790 Ma and was associated with the emplacement of a bimodal magmatic suite that underwent high-grade deformation prior to the emplacement of voluminous granite also at around 1790 Ma. The timing of D1/M1 coincides with the early stages of the Yambah Event, which is widely recognised in the southern Aileron Province, but has not previously been unequivocally shown to be associated with deformation . Subsequent pervasive reworking occurred over the interval 1600-1570 Ma, and was associated with long-lived granulite-grade metamorphism. The timing of this event coincides with the Chewings Orogeny which largely shaped the tectonic geology further west in the Reynolds and Anmatjira Ranges. During the Chewings Orogeny the c.1790 Ma D1 structures were transposed into a composite S1/S2 fabric. Map scale F2 folding is interpreted to have a shallow plunge suggesting that the S1 fabric may have originally been shallow dipping, raising the possibility that deformation was extensional in nature, and coeval with deposition of the nearby Reynolds Range Group which is constrained to the interval 1806-1785 Ma. Although inferred here to be Yambah aged, the timing constraints for D1 /M1 also overlap with the c. 1800 Ma Stafford Event which was associated with voluminous felsic magmatism, mafic magmatism and extreme geothermal gradient magmatism. This suggests that an extended period of extension, sedimentation, magmatism and deformation may have occurred at around 1800 Ma in the central Aileron Province.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2012
Then, M. "Constraints on the origin of early high-heat producing (U-Th enriched) granitic magmatism in central Australia." Thesis, 2016. http://hdl.handle.net/2440/121352.
Full textThe southern margin of central Australia is characterised by anomalous heat production, 3–5 times higher than global averages. Paleoproterozoic voluminous granitoid complexes in the region are important in the study of this anomalous heat flow. Ca.1800 Ma high-heat producing granites in Mt Boothby have A/NCK (molecular Al2O3/(CaO+Na2O+K2O)) ratios > 1, indicating a predominant origin from partial melting of metasedimentary rocks. The Boothby Orthogneiss is characterised by moderately negative Eu anomalies (Eu/Eu*: 0.03–0.43) and strong depletion in Ba, Rb, Nb and Sr. The enrichment of Ba and Rb relative to Sr and high K2O contents also support a metasedimentary source. The heat production values calculated for the Boothby Orthogneiss and the surrounding Lander formation show that the region is enriched in heat producing elements. The U-Pb zircon age data of inherited zircons in these granites are similar to the detrital zircons of the widespread outcropping; Lander formation. Nd values of -3.5 to 1.3 of the granites infer an evolved crustal source coupled with mixing of a newly mantle-derived component through lower crust assimilation. Zircon saturation temperatures calculated suggest that the Boothby intrusive complex was emplaced at 688–845oC, with a maximum temperature of 776oC, implying an arc environment with associated fluid-flux melting in the mantle wedge, ultimately controlled by subduction dynamics.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016