High gamma is related to the uranium content which is not related to TOC or gas in place.  Organic materials scavenge uranium and horde it.  But what if they had their uranium content removed or it never was there.  Recent developments indicate that a high gamma kick is not neccessary.  Its in the TOC.  Thats where the hydrocarbons are retained.

There is a play going on in Utah in the Mancos, the Bend Shale in the Palo Duro and one in Michigan in the Utica that do not have high gamma kicks but they are making good wells.  This requires a different approach.  Good samples or cores for analysis to determine TOC.    While the pack hunts for high gamma I am looking for the high TOC.

Coal bed methane reservoirs rely on water maintaining adsorbed methane in the coal by pressure.  Until the pressure is lowered to almost zero, in many cases, the methane gas will not flow to the well bore.  Recently, in some plays 3D or 2D seismic has been used to identify fracture trends.  This has had minimal success due to economics of coal bed methane resources.  Basically, the lower the cost for this type of resource play the better.  To date there is no verifiable evidence surface geochem was successful in a coal bed methane play.

In shale gas there are similar issues.  This type of resource is large and broad.  3D seismic is becoming successful because of the ability to identify fracutre and fault trends.  Surface geochem cannot identify in the subsurface where the frac or fault systems will be intersected by the drill bit.  This is why 3D is now being used aggressively and successfully. 

The level of detail sampling that needs to occur at the surface to find the fault or fracture trace is significiant and generally makes this method non-economic.  Also several of these plays have biogenic gas.  If the gas has migrated from the subsurface its difficult to separate from biogenic gas generated by biological activity at the surface.

 Surface Geochem is best used elsewhere .  

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