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A riveting expose of the global oil industry' s multi-decade conspiracy to muddy the waters around the science of climate change and use the Australian government to undermine worldwide efforts to address environmental devastation. Researched and written by one of Australia' s most fearless investigative journalists, Slick reveals how the US petroleum industry was warned about its environmental impacts back in the 1950s and yet went on to build the Australian oil industry, which in turn tried to drill the Great Barrier Reef, sought to strongarm governments, and joined a global effort to bury the science of climate change and delay action despite knowing the harms it would cause. Slick also tells the stories of fire and flood survivors, as well as of the activists engaged in a high-risk fight for the future of Australia and of the efforts being made to save ourselves from catastrophe. In this superb, in-depth work of journalism, Royce Kurmelovs provides an on-the-ground examination of how the fossil fuel industry captured Australia, and outlines what' s at stake for the survival of the planet and our democracy.
Fluid flow is fundamental to many geological processes, including the development of natural resources of hydrocarbons, ore deposits and water. Modelling of these processes requires information on the timing of fluid flow events and the interaction of fluids with surrounding rocks. In addition to isotopic methods, a diversity of approaches has been developed to assess the timing of events, including palaeomagnetism, fission track analysis and fluid inclusion studies. Many techniques also provide information on the duration of fluid flow events. The papers in this volume represent the range of approaches available to determine the dating and duration of fluid flow events and fluid-rock interaction: first overview of methods of dating fluid flow; examples of commercial application of dating methods; explanations of methodology suitable for advanced teaching; extensive bibliographies.
Collision between Australia and SE Asia began in the Early Miocene and reduced the former wide ocean between them to a complex passage which connects the Pacific and Indian Oceans. Today, the Indonesian Throughflow passes through this gateway and plays an important role in global thermohaline flow. The surrounding region contains the maximum global diversity for many marine and terrestrial organisms. Reconstruction of this geologically complex region is essential for understanding its role in oceanic and atmospheric circulation, climate impacts, and the origin of its biodiversity. The papers in this volume discuss the Palaeozoic to Cenozoic geological background to Australia and SE Asia collision. They provide the background for accounts of the modern Indonesian Throughflow and oceanographic changes since the Neogene, and consider aspects of the region's climate history--