HIGH-RESOLUTION SEISMIC REFLECTION SURVEYING USING LAND STREAMER FOR THE DELINEATION OF NEAR-SURFACE DEFORMATION STRUCTURE OF A CONCEALED FAULT.

2013 ◽  
Author(s):  
Tomio INAZAKI ◽  
Yoshinori MIYACHI ◽  
Atsushi URABE ◽  
Kyoko KAGOHARA
1993 ◽  
Vol 20 (15) ◽  
pp. 1615-1618 ◽  
Author(s):  
Edward W. Woolery ◽  
Ron L. Street ◽  
Zhenming Wang ◽  
James B. Harris

1992 ◽  
Vol 29 (9) ◽  
pp. 2038-2045 ◽  
Author(s):  
Erick Adam ◽  
Bernd Milkereit ◽  
Marianne Mareschal ◽  
Arthur E. Barnes ◽  
Claude Hubert ◽  
...  

Reprocessing of part of a Lithoprobe high-resolution seismic reflection line across the southern part of the Abitibi Belt has improved the imaging of shallow reflections and allowed correlation of the data with surface geology. Enhancement of early reflections was accomplished by focusing on the high-frequency content of the data. This improved resolution of reflections at two-way traveltime as early as 0.3 s and attenuated noise such as shear waves. The shallow reflections are interpreted as impedance contrasts at the contact between a metadiabase–diorite body and metavolcanics rocks. Offsets of the reflectors correlate with faults mapped at the surface and indicate a downdropped block, which may be of interest for mineral exploration.


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