RE: GRH tweet.9 Jun 2023 00:01
GRH is referring to salt deposits, which act like an extremely viscous liquid and slowly rise to the surface due to the weight of the overlying rocks - these form domes that penetrate those overlying strata - these are called diapirs. There is such a layer of Triassic salt underlying the Jurassic around Guercif, as well as many other gas & oil-bearing regions of the world. Hydrocarbons become pooled within reservoirs abutting these salt domes.
We had a private discussion on this potential a few months back. Since it was a private discussion, I will post only some of my side of the conversation, but I am sure Graham will not mind me saying that he was in general agreement.
"I haven't researched the Guercif Jurassic in as much depth, since it is mostly associated with oil rather than gas. Oil does not fit with the Predator energy transition positioning, and there is no refinery nor oil infrastructure in Morocco, so I have always assumed the oil opportunity will be taken up by a purchaser rather than by PRD.
You have mentioned the Zizi 1996 paper a few times – have you seen the follow-up by Sani & Zizi, 2000?
https://researchgate.net/publication/46603074_The_Neogene_Taza-Guercif_Basin
Fig 4 shows how complex the Jurassic stratigraphy can be over short distances, with huge changes in thickness and petrology. Some of this results from erosion of the Upper Jurassic giving a discontinuity before the deposition of the Tortonian, but the main controlling factor is the series of half-graben faults. Many of these have associated positive flower structures, providing favourable trapping potential.
Another trapping possibility is provided by diapirs of Triassic salt and/or mud penetrating the Jurassic. I suspect that these are a lot more common than is generally acknowledged – someone more familiar with the local geology suggested that just about every Jurassic anticline had a diapir at its core – the limited gravity data I have seen (trying to locate the source paper) would suggest that may be correct. The diapirism seems to be closely controlled by the fault geometry.
There are some good thicknesses of marl which should provide a good seal within the Jurassic strata. We know that of the two large reef structures identified by PRD, MOU-NW definitely has oil – this was confirmed back in 1924. As you know, carbonate material from strata analogous to MOU-NE has leached porosity development, and that indicates hydrocarbons close by."
and
from https://www.sciencedirect.com/science/article/abs/pii/S1464343X20300480
"Most of these anticlines are nucleated by diapiric Triassic evaporates (Benzaquen et al., 1965; Colletta, 1977)."
Colletta is a Swiss PhD thesis, can't locate the 1965 one."