Evaluation of a Distinct Sub-Play for Enhanced Exploration in an Emerging Petroleum Province, Bannu-Kohat Sub-Basin, Pakistan
Nadeem, Ahmad 1; Khan, Moin R.2
(1)Pakistan
Petroleum Ltd., Islamabad, Pakistan. (2) Pakistan Petroleum Ltd., Karachi,
Pakistan.
A prolific petroleum province, Bannu-Kohat sub-basin, has recently
emerged in the northwestern foreland basin of the Himalayan fold-&-thrust
belt in Pakistan. Creaming curve exhibits a bullish trend since first discovery
at Chanda only a decade ago. Gas and oil occur in multiple reservoirs. Although
new prospective structures continue to emerge, ambiguity surrounds the
definition of plays as distinct reservoir-seal
pairs and geological
inter-dependencies. Practical implications are: resources under-estimated,
misleading success/failure analysis of wells and ambiguous wellsite geology
decisions. This is an attempt to define key play and document its
sub-plays/part-plays within a sequence stratigraphic framework built through an
integration of outcrop, wireline log and seismic data. Key risk elements have
been assessed to draw Common Risk Segment (CRS) maps and prospectivity
corridors.
The Jurassic-Eocene sedimentary succession of interest was
deposited on the northwestern margin of the Indian plate in restricted to
shelfal marine setting in the form of six mega-sequences. The Lower Cretaceous
Chichali-Lumshiwal sequence, Upper Cretaceous Kawagarh sequence, Paleocene
Hangu-Lockhart sequence, and Paleocene-Eocene Patala-Panoba-MamiKhel
mega-sequence contain the reservoirs and seals of the key play of interest, the
Lumshiwal-Hangu-Lockhart play. Reservoirs are charged through juxtaposition
against prolific upper Paleocene Patala marine shale source. Regionally
extensive thick Panoba-Mamikhel shales and evaporites cap and laterally seal
the reservoirs in highly tectonized structural culminations to make the play
work. The Lumshiwal reservoir is fluvio-deltaic to strandplain shoreface
sandstone and correlates with the Lower Goru, a prolific play in the south.
Stacked Lumshiwal-Hangu sandstones with dual porosity (matrix-fracture) provide
key storage space. Overlying tight but fractured Lockhart Limestone serves to
drain the hydrocarbons.
Regional correlation and Wheeler diagram reveal a Shelf Margin Systems Tract in the form of calcareous shale and marly limestone deposited further basin-wards from the Lumshiwal coastal plains. Consequently, three stacked reservoir formations are split in the northwest to provide two sub-plays, Lumshiwal and Hangu-Lockhart, as also confirmed by the discoveries like Shekhan-1.Therefore, independent resource assessment of the two is essential. Wellsite decisions to drill deeper or abandon should also be made accordingly.
AAPG Search and Discovery Article #90135©2011 AAPG International Conference and Exhibition, Milan, Italy, 23-26 October 2011.