Origin, Characterisation and 3D Geometry of Dolomite Super-K Layers in the Permo-Triassic Khuff Formation (Middle-East)
F. Gisquet1, B. Caline1, A. Virgone1, J. Borgomano1
The Permo-Triassic Khuff Fm. is mainly composed by the alternation of limestone, dolomite and anhydrite bodies, over several hundred meters thick. Our study was focused on the upper part of the Khuff Formation, namely K4, K3, K2 and K1 reservoirs.
AAPG Search and Discovery Article #90188 ©GEO-2014, 11th Middle East Geosciences Conference and Exhibition, 10-12 March 2014, Manama, Bahrain