Table C Asia: Proposed New Refineries 相似文献
Table E Western Hemisphere: Proposed new refineries 相似文献
Table C Asia/Pacific: Proposed new Refineries 相似文献
NON-OPEC PRODUCERS 相似文献
- 1.
Cutting oriented. cores;
- 2.
Using dipmeters;
- 3.
Re-orienting in highly deviated holes;
- 4.
Using remanent palaeomagnetism.
The accuracy, costs and limitations of the methods are considered. 相似文献
- (i)
Identification of input and output variables. In this paper, the inputs are five compositional and textural parameters, namely: relative amounts of ductile grains, rigid grains and detrital matrix, to gether with grain size, and the Trask sorting coefficient. The output is either porosity or permeability.
- (ii)
Fuzzy clustering of output values.
- (iii)
Formation of membership grades of input data.
- (iv)
Generation of fuzzy rules; and
- (v)
Prediction via fuzzy inference.
Compared to statistical modelling (i. e. multiple regression analysis), fuzzy modelling is not only assumption-free but is also tolerant of outliers. Fuzzy modelling is capable of making both linguistic and numeric predictions based on qualitative knowledge and/ or quantitative data. Thus, fuzzy modelling is not only appropriate for the problem discussed here, but is also desirable for many geological problems characterized by non-numerical knowledge and imprecise information. 相似文献
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).
- (1)
Various species of Nummulites and planktonic foraminifera were identified in late Ypresian carbonates in the Kesra area and provided accurate biostratigraphic ages. Nummulitic limestones occur in the Chouabine and El Garia Formations representing deposition over a period of about 2Ma.
After correcting for the unreliable nature of data from non-commercial accumulations and then discounting the extreme high ends and low ends (
- •
P99 is 0.3MM brl or less in non-DHI oil plays and 4BCF or less in gas plays at normal depths;
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