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					 Other Shale Volume Methods All of
			these alternate shale volume methods are more than adequate, but
			suffer from strict limitations on their use. EPT and capture cross
			section are rare log curves.
 
			A number of useful shale volume methods have more restricted
                      The reader should take a moment to define
                      the parameters and work a hypothetical numerical example. 
					
					
					
					
					 Shale Volume from Electromagnetic Propagation
                          Attenuation The
                      electromagnetic propagation attenuation curve works well,
                      especially in thinly bedded sand-shale sequences because
					the tool has a bed resolution of 4 to 6 inches. Attenuation
                      increases with shale volume.
       1.
                      VSHept = (ATTEN - ATTEN_CLN) / (ATTEN_SHL - ATTEN_CLN)2:  VSHept = Min(1, Max(0, VSHept))
 
					
					 Shale Volume from Deep Resistivity The
                      deep resistivity sometimes can be used in hydrocarbon
					bearing zones, especially tar sands. Calculated shale volume
                      will be too high in water zones or swept zones when the
                      water is fairly salty (WS > 10000 ppm NaCl), so another
                      method, such as the SP or GR, should be used as well. Resistivity
                      decreases with higher shale volume. The method is very useful
                      in shallow shaly sands where kaolinite or feldspar makes
                      the gamma ray read high.
 The
			clean and shale resistivity values can be picked from suitable cross
			plots or from depth plots.  For the resistivity log method,
                      the use of the logarithm of the resistivity log values (and
                      base line values) works better than linear values, as follows: 
                            3. VSHresd = (log(RESD) - log(RESD_CLN)) / (log(RESD_SHL)
                      - log(RESD_CLN)) 4:  VSHresd = Min(1, Max(0, VSHresd))
 Note
                      that RESD_CLN is greater than RESD_SHL 
					
					 Shale Volume from Shallow Resistivity In
                      many shaly sands that are invaded with normal drilling mud
                      filtrate (Rmf >= 0.50 ohm-m), the shallow resistivity
                      may be a good shale indicator. Again, this is a very useful
                      method in feldspathic sandstones, and there is better bed
                      resolution than the deep resistivity. Do not use microlog
                      or microspherically focused log as RESS.
 
 5. VSHress = (log(RESS) - log(RESS_CLN)) / (log(RESS_SHL)
                      - log(RESS_CLN))
 6:  VSHress = Min(1, Max(0, VSHress))
 
					
					
					
					 Shale Volume from
					capture cross section Some
                      newer neutron logs produce a capture cross section curve
                      (SIGMA) which mimics a gamma ray log in shaly sands:
      
					7. VSHsig = (SIGMA – SIG_CLN) / (SIG_SHL – SIG_CLN)
					8:  VSHsig = Min(1, Max(0, VSHsig))
 All
                      cased hole thermal decay time logs display a SIGMA curve
                      as one of the primary measurements. Although there are hydrocarbon
                      effects, the curve can sometimes be used to overcome problems
                      with the gamma ray log, such as uranium precipitation on
                      casing or tubing, or missing GR log. 
					
					
					
					 Shale Volume from Photo Electric Effect This method is not very accurate as the spread between PE of
					quartz and shale is not large.
      
					9. VSHpe = (PE – PE_CLN) / (PE_SHL – PE_CLN) 10:  VSHpe = Min(1, Max(0, VSHpe))
 
					PE of
					quartz is between 1.6 to 1.8 and illite shale is near 3.5. l 
					
					
					
					 Even
                          More Methods The equations reproduced in the table below provide most of the
                      known relationships for calculating shale volume. This material
                      is reprinted courtesy of Dresser Atlas.
 
					 
 
  
 
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