Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications

The vertical or lithostatic stress is an important factor in tectonic and geomechanical studies and is commonly used in the prediction of pore pressures and fracture gradients. However, the vertical stress is not always calculated in situ and the approximation of 1.0 psi/ft (22.63 MPa/km) is often u...

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Main Authors: Tingay, Mark, Hillis, R., Morley, C., Swarbrick, R., Okpere, E.
Format: Journal Article
Published: Elsevier 2003
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/14155
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author Tingay, Mark
Hillis, R.
Morley, C.
Swarbrick, R.
Okpere, E.
author_facet Tingay, Mark
Hillis, R.
Morley, C.
Swarbrick, R.
Okpere, E.
author_sort Tingay, Mark
building Curtin Institutional Repository
collection Online Access
description The vertical or lithostatic stress is an important factor in tectonic and geomechanical studies and is commonly used in the prediction of pore pressures and fracture gradients. However, the vertical stress is not always calculated in situ and the approximation of 1.0 psi/ft (22.63 MPa/km) is often used for the vertical stress gradient. Vertical stress has been determined in 24 fields in the Baram Basin, Brunei, using density log and checkshot velocity survey data. The Baram Basin shows a variation in vertical stress gradient between 18.3 and 24.3 MPa/km at 1500 m depth below the surface. This variation has a significant effect on in situ stress related issues in field development such as wellbore stability and fracture stimulation. The variation is caused by a bulk rock density change of 2.48-2.07 g/cm3 from the hinterland of the delta to its front. Differential uplift and erosion of the delta hinterland and undercompaction associated with overpressure are the interpreted causes of the density and hence vertical stress variation.
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spelling curtin-20.500.11937-141552017-09-13T15:58:10Z Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications Tingay, Mark Hillis, R. Morley, C. Swarbrick, R. Okpere, E. Uplift Vertical stress Brunei The vertical or lithostatic stress is an important factor in tectonic and geomechanical studies and is commonly used in the prediction of pore pressures and fracture gradients. However, the vertical stress is not always calculated in situ and the approximation of 1.0 psi/ft (22.63 MPa/km) is often used for the vertical stress gradient. Vertical stress has been determined in 24 fields in the Baram Basin, Brunei, using density log and checkshot velocity survey data. The Baram Basin shows a variation in vertical stress gradient between 18.3 and 24.3 MPa/km at 1500 m depth below the surface. This variation has a significant effect on in situ stress related issues in field development such as wellbore stability and fracture stimulation. The variation is caused by a bulk rock density change of 2.48-2.07 g/cm3 from the hinterland of the delta to its front. Differential uplift and erosion of the delta hinterland and undercompaction associated with overpressure are the interpreted causes of the density and hence vertical stress variation. 2003 Journal Article http://hdl.handle.net/20.500.11937/14155 10.1016/j.marpetgeo.2003.10.003 Elsevier fulltext
spellingShingle Uplift
Vertical stress
Brunei
Tingay, Mark
Hillis, R.
Morley, C.
Swarbrick, R.
Okpere, E.
Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications
title Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications
title_full Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications
title_fullStr Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications
title_full_unstemmed Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications
title_short Variation in vertical stress in the Baram Basin, Brunei: tectonic and geomechanical implications
title_sort variation in vertical stress in the baram basin, brunei: tectonic and geomechanical implications
topic Uplift
Vertical stress
Brunei
url http://hdl.handle.net/20.500.11937/14155