Back to basicsIn that basin the second source rock was laid down in a restricted lacustrine setting then the Turonian Santonian Campanian over at Maka Central but across West of Corentyne in Guyana where Kawa is we have the Campanian and Santonian rising gradually to the south and the Eocene Paleocene deposits overlay giving a 6500 to 7000 meters of depth to source rock so over in Guyana there's a subtle difference in the geothermal gradient but the deposits of the Eocene -Paleocene are giving the pressure to the source rock to generate the Hydrocarbons..the channels of the lobes in that area also act as feeders where they incise the Santonian allowing hydrocarbons to migrate from NE to SW There is no major onshore deposits in Guyana .The AVO shows the Campanian to Santonian as good reservoir quality with DHIs ..so with vertical proximity to source rock n the added feeder channel system as a back up to move oil from high pressure Maka Central area to south west based on bouyancy ..with the seismic interpretation showing classic spill points etc etc..I don't have an issue being optimistic.So short at your own risk