From Gondwana to the Ice Age: The Geology of New Zealand Over the Last 100 Million Years - Bradshaw, John; Laird, Malcolm
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"Until about 100 million years ago, New Zealand lay on the Pacific-facing edge of the ancient supercontinent of Gondwana; the formation of our sedimentary rocks provides a fascinating view of the tectonic activity and changes since that time. This volume is the culmination of a comprehensive survey of New Zealand's Cretaceous-Cenozoic strata, begun in 1978, and presents an up-to-date synthesis and interpretation of regional sedimentary information from a variety of sources; the study has been expanded to include large areas of the continental shelf and beyond. Extensive references and indexing…mehr

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Produktbeschreibung
"Until about 100 million years ago, New Zealand lay on the Pacific-facing edge of the ancient supercontinent of Gondwana; the formation of our sedimentary rocks provides a fascinating view of the tectonic activity and changes since that time. This volume is the culmination of a comprehensive survey of New Zealand's Cretaceous-Cenozoic strata, begun in 1978, and presents an up-to-date synthesis and interpretation of regional sedimentary information from a variety of sources; the study has been expanded to include large areas of the continental shelf and beyond. Extensive references and indexing complete this essential work, a key resource for students, professional geologists and enthusiastic amateurs"--Back cover.
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Autorenporträt
John Bradshaw studied geology at London University and completed a PhD on the Precambrian and Paleozoic rocks of western Finistere in 1963. He joined the Geology Department of the University of Canterbury in 1966 where he remained until 2009. His research on Cretaceous tectonic changes and continental break-up led to further collaboration with Malcolm and the invitation to work with him on this book. John was a long-serving member of the Ross Dependency Research Committee and is a Fellow of the Royal Society of New Zealand. Malcolm Laird (1935-2015) graduated from Auckland University in 1962 and joined the New Zealand Geological Survey. In 1966 he was granted leave to complete a D.Phil. at Oxford, which focused on the sedimentology of Silurian rocks in western Ireland. On return to New Zealand, he commenced research on the sedimentary basins of the West Coast of the South Island; this later expanded to cover the whole of New Zealand and culminated in the management of a major project on the Cretaceous and Cenozoic basins of the New Zealand region. His work on New Zealand basins was complemented by studies of Paleozoic rocks in the Transantarctic Mountains and interpretation of Cenozoic rocks from offshore drilling in McMurdo Sound.