Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Journal of the Geological Society   Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Journal of the Geological Society; October 1980; v. 137; no. 5; p. 574; DOI: 10.1144/gsjgs.137.5.0574
© 1980 Geological Society of London
This Article
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 Search for Related Content

Article

Discussion

Mr. R. C. WALKER enquired whether the author had evaluated the extent of any structural instability the removal of such a large volume would have, and whether any researches had been conducted to consider the effect of solution of the large volume of evaporites, given that extensive fracturing associated with the proposed extraction techniques in an aquifer area might tend to increase solubility effects.

In reply, the AUTHOR stated: Research is being conducted on potential subsidence problems. In many cases there will be as much as 2000 ft (610m) of overburden covering the mined-out area, and, as a result, subsidence problems are not expected to be very severe. In terms of evaporites, most extraction will be in zones where soluble minerals have already been leached out, thus this problem should not be severe either. However, there are likely to be localized problems where shallow, unleached deposits are developed.

...

This 250-word extract was created in the absence of an abstract.







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