Belief and Proof6 Aug 2021 11:33
Morning all,
Believe what you wish and prove what you can.
I believe MOU1, MOU2,MOU4, GRF1, MSD1 & possibly KDH1 drilled in the locations they were, are all connected.
We know MOU1 is connected to MOU4 through the 2TGB sand and MOU1 is connected to MOU2 through the TGB 3 & 4 sands, so theoretically MOU1 is also connected to GRF1 through the TGB 3 & 4 sand as GRF1 also drilled this particular sand.
(an early presentation/RN does state one of the reasons for MOU1 drill is to prove connectivity between that and GRF1 structures/compartment, have to search)
Now what about Grf1 being connected to Msd1
This document on page 1354 under “Timings” states. (have to download)
https://af.booksc.org/book/64033701/2b7138
“This exercise was performed for two wells within the Neogene depocenter (GRF-1 and MSD-1), as well as
the surface stratigraphic column from the southern Guercif basin published by Krijgsman et al. (1999).
Both of the wells are located above the same structure, but lie about 5 km apart”.
There is evidence further down the document that both wells have the same porosity at the approximate same depths which also may go to show that they are connected.
The document also states that Kdh1 well was drilled on the structural high, page 1346 figure 4.
“Well KDH-1 was located on a structural high outside of the Neogene depocenter, whereas GRF-1 and MSD-1 were drilled within the depocenter”.
If you were to draw a straight line between drill sites MOU4 and KDH1 it would show that we are prospecting in a very large trough as called the Guercif Graben some 40kms long x 20kms wide with sediments up to 2.5kms thick.
That is what I believe.
This what I can prove.
It is well documented that there are missed payzones in the GRF1 well (Atlantic Oil, 2012 SLR,PRD et al.) from 10Bcf to 200Bcf of gas, we have all seen the detailed charts to prove porosity, permeability etc. and also that it would be possible to re-enter the well to extract the gas (2012 cpr)
We have the initial results from MOU1 as per the 6th July RN stating up to 1.7% C1 background gas down to target depth of 1159m (TGB3 & TGB4 Sands) and below 1159m in the lower Guebbas and Hoot, background gas of up to 1.5% C1 but with traces of heavier gases C2,C3 and C4 (TGB2 Sands)
We know through my earlier posts that these percentages of gas are good but have never seen another similar report or from the same location in Morocco to undoubtedly prove what we have found.
Hidden in plain sight, In a 2019 PRD presentation they revealed the mud log results (in French) from the GRF1 well, look at the % of C1 etc, at what depths and compare to what we revealed on the July 6th RN.
( Based on Background gas % and not the higher Formation gas %)
This proves If there’s payzones (extractable gas) in GRF1 there’s payzones in MOU1.
Page 22
https://www.predatoroilandgas.com/wp-content/uploads/2019/02/New-Presentation.pdf
AIMHO of course.
GLA
Wacky.