Funny old World23 Feb 2023 21:40
'The main seal rock of the upper most zone of interest is a mudstone that is laterally extensive and thick creating an impermeable barrier on both the upper and lower parts of the reservoir[10]. Relating this to the depositional environment, this would indicate that during the opening and closing of the sea, when the mudstone is present the deposits took place during deep sea burial. When the ocean started closing, the water became shallow creating the reservoir rock (Oligocene-Miocene turbidite sandstone) and when the ocean re-opened, more mudstone was created.The main seal rock of the upper most zone of interest is a mudstone that is laterally extensive and thick creating an impermeable barrier on both the upper and lower parts of the reservoir[10]. Relating this to the depositional environment, this would indicate that during the opening and closing of the sea, when the mudstone is present the deposits took place during deep sea burial. When the ocean started closing, the water became shallow creating the reservoir rock (Oligocene-Miocene turbidite sandstone) and when the ocean re-opened, more mudstone was created.The main seal rock of the upper most zone of interest is a mudstone that is laterally extensive and thick creating an impermeable barrier on both the upper and lower parts of the reservoir[10]. Relating this to the depositional environment, this would indicate that during the opening and closing of the sea, when the mudstone is present the deposits took place during deep sea burial. When the ocean started closing, the water became shallow creating the reservoir rock (Oligocene-Miocene turbidite sandstone) and when the ocean re-opened, more mudstone was created.'
The above is from a technical Paper... that should interest many
No...not about Guercif
It's about something a random old boy has droned on about...
A little gas field
Sorry...
I can't think of the name of it offhand
Regards
GRH
Oh ...I now remember
It's called Leviathan
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