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Thermochronology - the use of temperature-sensitive radiometric dating meth-ods to reconstruct the thermal histories of rocks - has proved to be an important means of constraining a wide variety of geological processes. Fission track and (U-Th)/He analyses of apatites, zircons and titanites are the best-established methods for reconstructing such histories over time scales of millions to hun-dreds of millions of years. The papers published in this volume are divided into two sections. The first sec-tion on 'New approaches in thermochronology', presents the most recent ad-vances of existing thermochronological methods and demonstrates the progress in the development of alternative thermochronometers and modelling tech-niques. The second section, 'Applied thermochronology', comprises original papers about denudation, long-term landscape evolution and detrital sources from the European Alps, northwestern Spain, the Ardennes, the Bohemian Massif, Fenno-scandia and Corsica. It also includes case studies from the Siberian Altai, Mozam-bique, South Africa and Dronning Maud Land (East Antarctica) and reports an ancient thermal anomaly within a regional fault in Japan.

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Alfred-Wegener-Institut für Polar- und Meeresforschung

Published: 1998

Total Pages: 240


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Antarctica preserves a rock record that spans three and a half billion years of history and has a remarkable story to tell about the evolution of our Earth, from the hottest crustal rocks yet found in an orogenic system, to the assembly and breakup of Gondwana in the Phanerozoic. This volume highlights our improved understanding of the tectonic events that have shaped Antarctica and how these potentially relate to supercontinent assembly and fragmentation. The internal constitution of the East Antarctic Shield is assessed using information available from the basement geology and from detritus preserved as Mesozoic sediments in the Trans Antarctic Mountains. Accretionary orogenesis along the proto-Pacific margin of Antarctica is examined and the volumes of intracrustal melting compared with juvenile magma additions in these complex orogenic systems assessed. This special volume demonstrates the diversity of approaches required to elucidate and understand crustal evolution and evaluate the supercontinent concept.