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Water is essential for all life forms. It is a fundamental resource necessary for socio-economic development and for ecological sustainability. Good quality water is becoming scarce due to population growth and associated industrial development and pollution particularly in towns and cities. It is timely that the sustainability and management of water resources is widely discussed noting that water can be used an unlimited number of times with proper treatment. The papers in Sustainability of Water Resources, were originally presented at a meeting at Murdoch University on 13-14 November 2002, where new and innovative methods of treatment, better understanding and assessment of resources and their supporting ecosystems, and proper management for conservation were explored. The meeting was preceded by a two day workshop on 'Water for Cities' and participants from the workshop from the Asia Pacific and Indian Ocean regions contributed to lively discussion at the conference
In this 1981 substantial work, M. J. Hambrey and W. B. Harland have assembled essays by leaders in the field of pre-Pleistocene glacial research. The work's various chapters review in depth the glacial records of Africa, Antarctica, Asia, Australasia, Europe, and North and South America.
Paralic reservoirs reflect a range of depositional environments including deltas, shoreline–shelf systems and estuaries. They provide the backbone of production in many mature basins, and contribute significantly to global conventional hydrocarbon production. However, the range of environments, together with relative sea-level and sediment supply changes, result in significant variability in their stratigraphic architecture and sedimentological heterogeneity, which translates into complex patterns of reservoir distribution and production that are challenging to predict, optimize and manage. This volume presents new research and developments in established approaches to the exploration and production of paralic reservoirs. The 13 papers in the volume are grouped into three thematic sections, which address: the sedimentological characterization of paralic reservoirs using subsurface data; lithological heterogeneity in paralic depositional systems arising from the influence of tidal currents; and paralic reservoir analogue studies of modern sediments and ancient outcrops. The volume demonstrates that heterogeneity in paralic reservoirs is increasingly well understood at all scales, but highlights gaps in our knowledge and areas of current research.
Many sedimentary basins worldwide contain extrusive and intrusive igneous rock sequences, and these rocks and associated magmatic processes can exert profound influences on a diverse range of basin processes and elements, including multiscale structural and tectonic development, heat flow, transport of hydrocarbons and other basinal fluids, and the hydraulic properties and integrity of reservoir and sealing units. Recent years have witnessed increased focus on improved understanding of igneous processes in basins to aid hydrocarbon exploration and development projects, and there is growing interest in the multifaceted role that igneous sequences in basins may play in the energy transition, for example as components of carbon capture and storage projects, and sources of geothermal energy, natural hydrogen and helium. This volume showcases state-of-the-art research from both academia and industry, drawing on global examples and addressing reservoir-to-plate scales, providing critical new data, knowledge and technological capabilities that highlight the opportunities, complexities and potential pitfalls associated with unlocking the energy resources of sedimentary basins impacted by igneous processes.
"This volume summarizes new developments in understanding the longest-lived icehouse period in Phanerozoic Earth history, the late Paleozoic ice age. Resolving the Late Paleozoic Ice Age in Time and Space provides summaries of existing and new data from the various Gondwanan continental relics, and also reviews stratigraphic successions from the paleotropical and temperate regions of Laurussia that preserve an indirect record of glaciation. It addresses the extent to which records of glaciation indicate protracted, long-term climatic austerity, as opposed to fluctuating, more dynamic climate, and provides new constraints on the timing of glaciation. Additionally, it tackles questions of synchroneity of glaciation across the various Gondwanan continental relics, and timing relationships between near-field and far-field records at greater levels of resolution than has been possible previously. Results point toward a dynamic icehouse regime that is comparable to the Cenozoic icehouse, and away from traditional interpretations of the late Paleozoic ice age as a single, protracted event that involved stable, long-lived ice centers."--Publisher's website.