Ancient Orogens and Modern Analogues (Geological Society by J. B. Murphy, J. D. Keppie, A. J. Hynes

By J. B. Murphy, J. D. Keppie, A. J. Hynes

Plate tectonics supply a unifying conceptual framework for the knowledge of Phanerozoic orogens. extra controversially, contemporary syntheses practice those ideas way back to the Early Archaean. Many old orogens are, despite the fact that, poorly preserved and the tactics accountable for them are usually not good understood. the results of tactics resembling delamination, subduction of oceanic and aseismic ridges, overriding of plumes and subduction erosion are hardly ever pointed out in historical orogens, even if they've got a profound impression on Cenozoic orogens. in spite of the fact that, deeply eroded old orogens supply insights into the hidden roots of contemporary orogens. contemporary advances in analytical suggestions, in addition to in fields similar to geodynamics, have supplied clean insights into old orogenic belts, in order that practical sleek analogies can now be utilized. This unique ebook deals up to date stories and types for the most vital orogenic belts constructed during the last 2.5 billion years of Earth history.The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on the planet, and one of many greatest publishers within the Earth sciences.The Society publishes quite a lot of top quality peer-reviewed titles for teachers and pros operating within the geosciences, and enjoys an enviable overseas acceptance for the standard of its work.The many parts within which we post in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reviews and geochemistry-Remote sensing-History of geology-Regional geology courses

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Additional info for Ancient Orogens and Modern Analogues (Geological Society Special Publication No. 327)

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J. N. 2005. 40Ar/39Ar ages of silicic rocks in the Tauranga-Kaimai area, New Zealand: dating the transition between volcanism in the Coromandel Arc and the Taupo Volcanic Zone. New Zealand Journal of Geology and Geophysics, 48, 459–469. B ROWN , S. J. A. 1994. Geology and geochemistry of the Wkahamaru-group ignimbrites, and associated rhyolite domes, Taupo Volcanic Zone, New Zealand. PhD thesis, University of Canterbury, Christchurch, New Zealand. B ROWN , S. J. , S MITH , R. T. & C OLE , J. W.

W EAVER , S. , B RIGGS , R. M. & P RINGLE , M. S. 1995. Chronology and dynamics of a large silicic magmatic system, Central Taupo Volcanic Zone, New Zealand. Geology, 23, 13– 16. H UNT , T. M. 1992. Gravity studies in the Rotorua area, New Zealand. Geothermics, 21, 65–74. J URADO -C HICHAY , Z. & W ALKER , G. P. L. 2000. Stratigraphy and dispersal of the Mangaone Subgroup pyroclastic deposits, Okataina Volcanic Centre, New Zealand. Journal of Volcanology and Geothermal Research, 104, 319 –383.

W ILSON , C. J. N. 1995. An outline geochemistry of rhyolite eruptives from Taupo volcanic centre, New Zealand. Journal of Volcanology and Geothermal Research, 68, 153– 175. S UTTON , A. , W ILSON , C. J. N. & C HARLIER , B. L. A. 2000. Late Quaternary evolution of a hyperactive rhyolite magmatic system: taupo volcanic centre, New Zealand. Journal of the Geological Society, London, 157, 537– 552. V ILLAMOR , P. & B ERRYMAN , K. 2001. A late Quaternary extension rate in the Taupo Volcanic Zone, New Zealand, derived from fault slip rate.

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