552 research outputs found

    Behavior of the collective rotor in wobbling motion

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    The behavior of the collective rotor in wobbling motion is investigated within the particle-rotor model for the nucleus 135^{135}Pr by transforming the wave functions from the KK-representation to the RR-representation. After reproducing the experimental energy spectra and wobbling frequencies, the evolution of the wobbling mode in 135^{135}Pr, from transverse at low spins to longitudinal at high spins, is illustrated by the distributions of the total angular momentum in the intrinsic reference frame (azimuthal plot). Finally, the coupling schemes of the angular momenta of the rotor and the high-jj particle for transverse and longitudinal wobbling are obtained from the analysis of the probability distributions of the rotor angular momentum (RR-plots) and their projections onto the three principal axes (KRK_R-plots).Comment: 21 pages, 9 page

    “I Knew the Mechanics of Hip”: Fashioning Bodies in the Works of Joni Mitchell, 1968 - 1979

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    Since the late 1960s, Joni Mitchell has been best known for her remarkable music: her voice, compelling lyrics, and unusual guitar tunings, all of which have conveyed sentiments of her generation and have remained relevant to later generations. Although her lyrics and album covers are replete with references to fashion, textiles, dress, and appearance, they have not been critically analyzed in relation to her status as a cultural icon. The fashion industry is clearly aware of this status, as evidenced, for example, by her inclusion in a 2015 Yves St. Laurent campaign. In our study, we ask: (1) What does Mitchell’s music convey about fashion, textiles, dress, and appearance? (2) What fashion philosophies and themes are found in her vocal and visual arts? To answer these questions, we completed a content analysis of Mitchell’s lyrics, alongside a visual analysis of her album art. By studying the period of 1968 to 1979, our research captures the epoch of her greatest radio influence and record sales, and identifies the messages and fashion philosophies threaded throughout her songs and artwork

    Mantle Sources and Geochemical Evolution of the Picture Gorge Basalt, Columbia River Basalt Group

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    The Columbia River Basalt Group (CRBG) is the youngest continental flood basalt province, proposed to be sourced from the deep-seated plume that currently resides underneath Yellowstone National Park. If so, the earliest erupted basalts from this province, such as those in the Picture Gorge Basalt (PGB), aid in understanding and modeling plume impingement and the subsequent evolution of basaltic volcanism. Using geochemical and isotopic data, this study explores potential mantle sources and magma evolution of the PGB. Long known geochemical signatures of the PGB include overall large ion lithophile element (LILE) enrichment and relative depletion of high field strength elements (HFSE) typical of other CRBG main-phase units. Basaltic samples of the PGB have 87Sr/86Sr ratios on the low end of the range displayed by other CRBG lavas and mantle-like δ18O values. The relatively strong enrichment of LILE and depletion of HFSE coupled with depleted isotopic signatures suggest a metasomatized upper mantle as the most likely magmatic source for the PGB. Previous geochemical modeling of the PGB utilized the composition of two high-MgO primitive dikes exposed in the northern portion of the Monument Dike swarm as parental melt. However, fractionation of these dike compositions cannot generate the compositional variability illustrated by basaltic lavas and dikes of the PGB. This study identifies a second potential parental PGB composition best represented by basaltic flows in the extended spatial distribution of the PGB. This composition also better reflects the lowest stratigraphic flows identified in the previously mapped extent of the PGB. Age data reveal that PGB lavas erupted first and throughout eruptions of main-phase CRBG units (Steens, Imnaha, Grande Ronde Basalt). Combining geochemical signals with these age data indicates cyclical patterns in the amounts of contributing mantle components. Eruption of PGB material occurred in two pulses, demonstrated by a ~0.4 Ma temporal gap in reported ages, 16.62 to 16.23 Ma. Coupling ages with observed geochemical signals, including relative elemental abundances of LILE, indicates increased influence of a more primitive, potentially plume-like source with time
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