Porosity and permeability relationships of the Lekhwair and Lower Kharaib Formations
dc.contributor.advisor
Haszeldine, Stuart
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dc.contributor.advisor
Wood, Rachel
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dc.contributor.author
Cox, Peter A.
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dc.contributor.sponsor
Scottish Funding Council for ECOSSE which is a part of the
Edinburgh Research Partnership in Engineering and Mathematics (ERPem)
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dc.date.accessioned
2016-08-23T15:42:53Z
dc.date.available
2016-08-23T15:42:53Z
dc.date.issued
2011-11-24
dc.description.abstract
Up to 60% of the World’s oil is now within carbonates, with over 50% in
the Middle East. Many existing carbonate fields have very low oil recoveries due to
multiple scales of pore heterogeneity. To secure better recoveries the controls from
deposition and diagenesis towards the origin of carbonate pore heterogeneity needs
better understanding. To provide good sample support, three High frequency Cycle’s
were sampled (2 from the Lekhwair Formation and the third being the Lower
Kharaib Formation) from an offshore field (Abu Dhabi) along a southwest-northeast
transect, encompassing the oil leg, transition zone, water leg, the field crest and two
opposing flanks.
With respect to deposition, the 4th order Sequence Boundaries’ (hardgrounds) and
the Maximum Flooding Surface’s were correlated across the field, within the
sequence stratigraphic framework, showing that each HFC, of the Lekhwair
Formation, contains laterally continuous reservoirs (4th order HST’s) which are
compartmentalised above and below by impermeable seals (4th order TST’s). The
Lower Kharaib Formation shows significant shoaling producing the shallowest
platform (prolonged 3rd order TST) and the best connected reservoir facies.
With respect to diagenesis, δ 18O isotopes trends, from calcite cement zones within
macrocements from the water and oil legs, in comparison with oil inclusion
abundances suggest that oil charge reduced cementation in the crest macropores.
Stylolitisation in the water leg at deep burial provided solutes for new cement
nucleation causing near complete macropore occlusion.
The most open micropore networks coincide with the highest
porosity/permeability relationships at the mid-late HST’s of each HFC. Considering
these areas could be lower grade reservoirs, and that pore characterisation by Lucia
(1999) does not include identifying and quantifying micropores, a new ‘Micropore
model’ (using elements from the Petrotype atlas method) is devised. This new
method highlights micropore-dominated areas alongside macropore-dominated areas
within specific reservoir horizons. This provides information of pore heterogeneity at
several scales within a carbonate reservoir and may determine the method for oil
extraction and increase oil recovery from both the Lekhwair and Lower Kharaib
Formations.
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dc.identifier.uri
http://hdl.handle.net/1842/16161
dc.language.iso
en
dc.publisher
The University of Edinburgh
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dc.relation.hasversion
Cox, P. A., Wood, R. A., Dickson, J. A. D., Al-Rougha, H. B., Shebl, H. & Corbett, P. W. M.: (2010): Dynamics of cementation in response to oil charge: Evidence from a Cretaceous carbonate field, U.A.E. Sedimentary Geology: 228: p246-254.
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dc.subject
carbonate fields
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dc.subject
carbonate pore heterogeneity
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dc.subject
High frequency Cycle
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dc.subject
HFCs
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dc.subject
HSH's
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dc.subject
pore heterogeneity
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dc.subject
oil recovery
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dc.title
Porosity and permeability relationships of the Lekhwair and Lower Kharaib Formations
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dc.title.alternative
The porosity and permeability relationships of the Lekhwair and Lower Kharaib Formations
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dc.type
Thesis or Dissertation
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dc.type.qualificationlevel
Doctoral
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dc.type.qualificationname
PhD Doctor of Philosophy
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