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Mineralogical Magazine; April 2008; v. 72; no. 2; p. 651
© 2008 Mineralogical Society of Great Britain and Ireland
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PREFACE

A. K. Kleppe1, A. Anderson2 and J.-L. Hazemann3

1 Diamond Light Source, Harwell Science and Innovation Campus, Didcot, Oxfordshire OX11 0DE and Department of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR, UK
2 Department of Earth Sciences, St. Francis Xavier University, Nova Scotia, B2G 2W5, Canada
3 Institut Néel, CNRS, 25 Avenue des Martyrs, 38042 Grenoble Cedex 9, France

The first 20% of the full text of this article appears below.

Progress in the Earth sciences and mineralogy in particular is, and has always been, intimately linked to the development of powerful analytical techniques. Today, to an ever-increasing extent, the study of the physical and chemical properties of Earth and planetary materials requires the availability of large-scale facilities that involve probing particles with radiation of specific characteristics, such as high brilliance. During this decade the European synchrotron landscape is undergoing significant changes. New, national, large-scale facilities are opening for users at many locations around Europe: e.g. in the UK, Diamond Light Source opened at the beginning . . . [Full Text of this Article]







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
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