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The Baikalide–Altaid, Transbaikal–Mongolian and North Pacific orogenic collages: similarity and diversity of structural patterns and metallogenic zoning

By
Alexander Yakubchuk
Alexander Yakubchuk
Centre for Russian and Central Asian Mineral Studies, Department of Mineralogy, Natural History Museum, Cromwell Road, London SW7 5BD, UK, a.yakubchuk@nhm.ac.uk
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Published:
January 01, 2002

Abstract

The Baikalide–Altaid, Transbaikal–Mongolian and North Pacific orogenic collages consist of several oroclinally bent magmatic arcs separated by accretionary complexes and ophiolitic sutures located between the major cratons. The tectonic and metallogenic patterns of these collages are principally similar as they were formed as a result of rotation of the surrounding cratons and strike-slip translation along the former convergent margins.

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Contents

Geological Society, London, Special Publications

The Timing and Location of Major Ore Deposits in an Evolving Orogen

D. J. Blundell
D. J. Blundell
Royal Holloway, University of London, UK
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F. Neubauer
F. Neubauer
University of Salzburg, Austria
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A. von Quadt
A. von Quadt
ETH-Z, Zurich, Switzerland
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Geological Society of London
Volume
204
ISBN electronic:
9781862394520
Publication date:
January 01, 2002

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