During the 2006 conference call, Ben Law was asked what he thought of the quality of the rocks in the Mako trough. He answered with this:

"I think what, going into this program, we've found is that, for one thing, I just would like to say that the geologic age of these rocks is very young compared to anything in the US or Canada of a similar kind of accumulation. What that really implies is that we're dealing with rock sequences here that haven't been exposed to a lot of structural deformation and rock-water interactions that collectively degrade reservoir characteristics. In fact, the nets confirm by the core data from the Hod Well that indicates that we are in a sequence that has at least 10 times better permeability. Permeability is just the ability of fluids to move through a matrix. You can measure it in darcies or millidarcies. In the Makó Trough, the Szolnok—particularly the Szolnok—and the Endröd have better reservoir characteristics to start with"

Here's a permeability chart:

If you thought Susan Boyles performance was jaw dropping, check this out:

http://www.bmmernokikamara.hu/wp-con...

This info certainly isn't NI51-101 compliant, so enjoy at your own risk :)