Thank you for the very informative video Patrick. As an RE, it discusses a very important aspect of model building and some of the QA/QC that needs to be done. The video also shows actual FZI data overlaid on the GHE plots showing the distribution of different systems.
Thank you for the clear explanation on petrotyping exercise. Working in Miocene carbonate, I can totally relate to the carbonate plot that you just showed. Been following your work Pat, huge fan!
Thanks for the video, however i am a bit confused here. In the chart that shows the poro perm and the different flow zones, lets say the Shuaiba you have shown, all individual FZI's have a very wide range of poro and perm values, i mean the rock that has a very high poro & very high perm (sample located upper right in color x) falls under the same rock type that has very low poro & very low perm (sample located lower left in color x); meaning both are classified in the same FZI, how is that possible? I didnt get that...
Thank you for the very informative video Patrick. As an RE, it discusses a very important aspect of model building and some of the QA/QC that needs to be done. The video also shows actual FZI data overlaid on the GHE plots showing the distribution of different systems.
Thank you for the clear explanation on petrotyping exercise. Working in Miocene carbonate, I can totally relate to the carbonate plot that you just showed.
Been following your work Pat, huge fan!
Thanks for the video, however i am a bit confused here. In the chart that shows the poro perm and the different flow zones, lets say the Shuaiba you have shown, all individual FZI's have a very wide range of poro and perm values, i mean the rock that has a very high poro & very high perm (sample located upper right in color x) falls under the same rock type that has very low poro & very low perm (sample located lower left in color x); meaning both are classified in the same FZI, how is that possible? I didnt get that...
Good sadly I am about to highlight the failings of legacy cOre analysis on MEast carbonates !also rock type often varies along the same H layer !