Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Journal of Environmental & Engineering Geophysics Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Journal of Environmental & Engineering Geophysics; June 2006; v. 11; issue. p. 143-150; DOI: 10.2113/JEEG11.2.143
© 2006 Environmental & Engineering Geophysical Society
This Article
Right arrow Figures Only
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 Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Gu, H.
Right arrow Articles by Wang, Y.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Investigation of Fractures Using Seismic Computerized Crosshole Tomography

Hanming Gu , Chengguo Cai and Yunsheng Wang

Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan, Hubei, 30074, P.R. China Email: guhanming{at}263.net

Geological features such as fractures and voids pose potential hazards to the safe construction and operation of tunnels. The high resolution of seismic computerized tomography has been successfully applied to the detection of such features prior to the construction of a railway tunnel through Qiyue Mountain in central China. Data were acquired using three boreholes drilled to 280 m in Triassic carbonates and interpreted using seismic computerized tomography (CT) based on ray theory. We used a sparker source in one borehole and an array of hydrophones in a second borehole as receivers. First arrival times were picked automatically, and we applied the algorithm SIRT to reconstruct the variation of seismic velocity between the boreholes. Combining the results with information from engineering drilling, we were able to map precisely the distribution of fractures, rock fragmentation and small voids in the plane defined by the three wells. The results show that there are four linear low-velocity features, which are interpreted as fracture zones. Discrete low-velocity anomalies along these fracture zones are interpreted as small voids. These are consistent with the drilling results. The results provide an excellent example of the applicability of seismic elastic CT in mapping geological hazards such as voids and fractures.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Environmental & Engineering Geophysical Society