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1.
A review of four simple techniques used to re-orient conventional cores back to theri in-situ position in presented. Cores can be oriented by: The accuracy, costs and limitations of the methods are considered. 相似文献
2.
High-resolution (biomarker) geochemistry combined with other geochemical data has been used to investigate the genetic relationships of 14 crude oil samples from the Iranian sector of the Persian Gulf, and to provide information on the lithologies, palaeo-depositional environments and probable ages of the respective source rocks. Oil samples from the Resalat, Salman, Sirri A, Sirri C, Sirri D and Sirri E fields in the SE of the Gulf, and the Foroozan, Bahregansar, Hendijan, Abouzar, Doroud and Nowrouz fields in the NW of the Gulf were investigated. Results indicate that the studied oils belong to three genetic groups: - (i)
Group 1 oils (Resalat and Salman fields) were sourced from Jurassic or older, shaly source rocks deposited in a relatively oxic environment; - (ii)
Group 2 oils (Nowrouz, Doroud and Foroozan oilfields) originated from Jurassic or older carbonate-rich source rocks deposited in an anoxic environment; - (iii)
Group 3 oils, which, according to biomarker parameters, were probably sourced from Middle Cretaceous calcareous shales. Two subgroups are recognised: subgroup 3A oils were sampled from oilfields located in the NW of the Gulf (Hendijan, Bahregansar and Abouzar), and subgroup 3B oils came from the south (Sirri A, Sirri C, Sirri D and Sirri E fields).
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3.
Eocene nummulite deposits along the southern Tethys margin locally constitute important hydrocarbon reservoir rocks. In order to understand the heterogeneity of these complex reservoirs, we have carried out a detailed field study of the nummulite limestones which crop out at the Kesra Plateau in Central Tunisia. The main contributions of this paper can be summarised as follows:
4.
One problem with the inversion of transient well test data is that it can yield a non-unique solution. The uncertainty resulting from this type of approach can only be resolved by considering information from another source such as geology. Geological information will help to define the interpretation model which will ensure the correct analysis of the well test data. The results of well test analyses are of little value to reservoir characterisation and modelling unless they can be explained from a geological point of view. This last step is what we refer to here as geological interpretation. Other sources of information which can help with well test analyses come from seismic surveys and petrophysics. Modern well test interpretation therefore consists of two major steps: analysis of the well test data; and interpretation of the results. In detail, this should include the following:
5.
Problems with measuring fault slip in the subsurface can sometimes be overcome by using subsurface structural contour maps constructed from well logs and seismic information. These maps are useful for estimating fault slip since fault motion commonly causes the dislocation of structural contours. The dislocation of a contour is defined here as the distance in the direction of fault strike between two contours which have the same value on both sides of a fault. This dislocation can be estimated for tilted beds and folded beds as follows: - (i)
If a dip-slip fault offsets a tilted bed, the dislocation (Sc) of contours can be estimated from the vertical component (Sv) of the fault slip and the dip (β) of the bedding according to the following relationship: Sc= Sv/tan β. Since Sc and β can be measured from a contour map, the vertical component of fault slip can be obtained from this equation. If a strike-slip fault offsets a tilted bed, the dislocation (Scs) of contours is equal to the strike-slip of the fault (Sc), that is, Scs= Ss.
6.
Mathematical theory and empirical data show that discovery sizes from mature plays have lognormal distributions. This allows a simple transformation to be used that converts lognormal trends to straight lines from which valuable statistical data on exploration potential is derived. After correcting for the unreliable nature of data from non-commercial accumulations and then discounting the extreme high ends and low ends ( P1), discovery size distributions from a variety of mature plays outside the Middle East show certain common properties that help constrain reserves ranges in individual prospects and new play fairways. These are:
7.
This paper investigates the sedimentological response of the Tertiary Pindos and Mesohellenic Basins to localized tectonic and eustatic sea-level changes in a submarine setting dominated by turbidite deposition. Five composite stratigraphic cross-sections were compiled from field data, three in the Pindos Basin and two in the Mesohellenic Basin; 45 samples were dated by means of nannofossil bio stratigraphy. On the basis of these field studies, we relate observed changes in depositional environment to eustatic sea-level changes and to activity on local thrusts. Between the early Eocene and the late Miocene, tectonically-driven subsidence in both basins was generally more significant than eustatic variations in controlling depositional patterns. However, depositional conditions can be related to eustatic changes at four specific times:
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