Stoops have a look on the CTP website. Go to the downloads tab then go to other documents and at the bottom is a CBM and GTL document finished in 2007. in there is a report on the horn valley siltstone As it is described as a " source" rock . Under7.3 stratigraphy. It's not the good document I saw yesterday ( it buried in a gov website somewhere just can't remember how I got there) but it virtually says the same thing and the diagrams of the geo layers on the other explain it a bit better ( to a layman anyway) I hope this helps once I find the other one I will let you know.
And there is a distinct possibility that if what he is alluding to in regards to the length and volume of this shale play, it is a lot bigger than what everyone thinks. How many players are there involved with the eagle ford shale, Bakken or niobara ? One thing I do know is that the tenements are a hell of a lot smaller. And we can count one one hand who has access to this this shale on one hand minus a finger or two.
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500klm, 150m and 9.5% organics means what?, page-11
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