Difference between revisions of "Smear-gouge ratio"

From AAPG Wiki
Jump to navigation Jump to search
 
(One intermediate revision by the same user not shown)
Line 1: Line 1:
Smear-gouge ratio is the ratio of sand to shale that has moved past some critical portion of the fault plane.<ref>Skerlec, G. M., 1996, Risking fault seal in the Gulf Coast (abs.): AAPG Annual Convention Program and Abstracts, v. 5,   
+
{{publication
p. A131.</ref> Although not simply relatable to the shale gouge ratio, the smear gouge ratio varies in an inverse manner; i.e., high shale gouge ratio corresponds to low smear gouge ratio and vice versa.
+
| image  = Bulltein-Jun1997.jpg
 +
| width  = 120px
 +
| series  = ''AAPG Bulletin,'' June 1997
 +
| title  = Quantitative Fault Seal Prediction
 +
| part    =
 +
| chapter =
 +
| frompg  = 897
 +
| topg    = 917
 +
| author  = G. Yielding, B. Freeman, and D. T. Needham
 +
| link    = http://archives.datapages.com/data/bulletns/1997/06jun/0897/0897.htm
 +
| pdf    =
 +
| store  =
 +
| isbn    =
 +
}}
 +
 
 +
Smear-gouge ratio is the ratio of sand to [[shale]] that has moved past some critical portion of the fault plane.<ref>Skerlec, G. M., 1996, Risking fault seal in the Gulf Coast (abs.): AAPG Annual Convention Program and Abstracts, v. 5,  p. A131.</ref> Although not simply relatable to the shale gouge ratio, the smear gouge ratio varies in an inverse manner; i.e., high shale gouge ratio corresponds to low smear gouge ratio and vice versa.
  
 
Both ratios are commonly called SGR.
 
Both ratios are commonly called SGR.
 
==Further Reading==
 
* Yielding, G., B. Freeman, and D. T. Needham, 1997, [http://archives.datapages.com/data/bulletns/1997/06jun/0897/0897.htm Quantitative Fault Seal Prediction]: AAPG Bulletin, vol. 81, no. 6, p 897.
 
  
 
==References==
 
==References==
 
{{reflist}}
 
{{reflist}}

Latest revision as of 13:49, 18 March 2019

Quantitative Fault Seal Prediction
Series AAPG Bulletin, June 1997
Author G. Yielding, B. Freeman, and D. T. Needham
Link Web page

Smear-gouge ratio is the ratio of sand to shale that has moved past some critical portion of the fault plane.[1] Although not simply relatable to the shale gouge ratio, the smear gouge ratio varies in an inverse manner; i.e., high shale gouge ratio corresponds to low smear gouge ratio and vice versa.

Both ratios are commonly called SGR.

References

  1. Skerlec, G. M., 1996, Risking fault seal in the Gulf Coast (abs.): AAPG Annual Convention Program and Abstracts, v. 5, p. A131.