Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Economic Geology Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Economic Geology; June-July; v. 102; no. 4; p. 762; DOI: 10.2113/gsecongeo.102.4.762
© 2007 Society of Economic Geologists
This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Galley, A.
Right arrow Search for Related Content

Book Reviews

Physical Geology of High-Level Magmatic Systems.

CHRISTOPHER BREITKREUZ and NICK PETFORD, EDITORS. Pp. 262. Geological Society of London, Special Publication 234. 2004. ISBN 1-86239-169-6. Price Members, £40.00, Other Societies, £48.00, Nonmembers, £80.00.

Alan Galley

Geological Survey of Canada, Ottawa, Ontario

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

The 14 papers contained within this volume are the product of a two-day workshop held at TU Bergakademie Freiberg in 2002 on the physical geology of subvolcanic systems. The recognition of subvolcanic sill complexes and an understanding of their emplacement histories are of critical importance to economic geologists with an interest in a wide variety of magmatic-hydrothermal ore deposits. Many of the papers in the volume describe the geologic setting, physical attributes, and emplacement histories of high-level sill and dike complexes within a number of European late Paleozoic sedimentary basins. These basins formed in a number of tectonic settings ranging from continental foreland extension during late orogenesis through to oceanic back-arc extension and magmatism. Two exceptions are papers describing Neogene to Recent magmatism and caldera formation in the anorogenic oceanic . . . [Full Text of this Article]







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Society of Economic Geologists