gas in the elang-plover, gas in sandstone abov, page-60

oilman, its a little tricky because most of the cross-sections are from H-2 to H-1, whereas HS-1 is more to the west from this transect, and is also close to a structural high.

So it is deeper (sequence wise), but probably less than the 200m. However, the overlying sequence in the southern block which correlate with the northern block also appear to be reservoir quality sands which are gas charged (the cored zones), so only upside from a volume perspective.

From a well-control, tie-in perspective, you are more than likely right.