787 resultados para Petrology Queensland Monsildale

em University of Queensland eSpace - Australia


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The Upper Newlands Seam in the northern Bowen Basin, Queensland, Australia consists of six benches (A-F) that have different petrographic assemblages. Benches C and E contain relatively abundant inertodetrinite and mineral matter, as well as anomalously high reflectance values; these characteristics support a largely allochthonous, detrital origin for the C and E benches. Fractures and cleats in the seam show a consistent orientation of northeast- southwest for face cleats, and a wide range of orientations for fractures. Cleat systems are well developed in bright bands, with poor continuity in the dull coal. Both maceral content and cleat character are suggested to influence gas drainage in the Upper Newlands Seam. A pronounced positive correlation between vitrinite abundance and gas desorption data suggests more efficient drainage from benches with abundant vitrinite. Conversely, inertinite-rich benches are suggested to have less efficient drainage, and possibly retain gas within pore spaces, which could increase the outburst potential of the coal. (C) 2001 Elsevier Science BN. All rights reserved.

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As seen from Blair Road.

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As seen from Balir Road.

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Formal elevation facing University of Queensland entrance roads.

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As seen from informal courtyard; Duhig Tower beyond.

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Formal elevation facing University of Queensland entrance roads.

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Formal elevation facing University of Queensland entrance roads.

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Formal elevation facing University of Queensland entrance roads.

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Entry from landscaped amphitheatre area.

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Open-ended folded sheet metal gutter.