Central Graben
31 December 2012

Orchid exploration. Dip-closure over salt swell with Upper Paleocene Andrew Sandstone and Lower Paleocene/Upper Cretaceous Ekofisk/Tor chalk at c. 7,900- 8,100 ft. Strong amplitudes and flat event in Chalk indicate porosity preservation resulting from early oil charge. Well was junked and re-spudded.

Operator(s): 
Formation(s):