Reservoir Evaluation of
32,99 €
inkl. MwSt.
Versandkostenfrei*
Versandfertig in 6-10 Tagen
payback
16 °P sammeln
  • Broschiertes Buch

Reservoirs in Banghan field are evaluated using well logs, Seismic, biofacies and core data. To understand a reservoir, one must know the structures that are present within a field that may serve as trapping mechanism for hydrocarbon. Using seismic, the faults, fault polygon, structural map, surfaces and regional dips were determined. Well logs were use to identify chrono unit, lithofacies, lithologies and correlate them within Banghan field. Biofacies data were used to define also chrono unit, chrono surface and lithologic age. Sequence stratigraphic analysis and cross section of Banghan…mehr

Andere Kunden interessierten sich auch für
Produktbeschreibung
Reservoirs in Banghan field are evaluated using well logs, Seismic, biofacies and core data. To understand a reservoir, one must know the structures that are present within a field that may serve as trapping mechanism for hydrocarbon. Using seismic, the faults, fault polygon, structural map, surfaces and regional dips were determined. Well logs were use to identify chrono unit, lithofacies, lithologies and correlate them within Banghan field. Biofacies data were used to define also chrono unit, chrono surface and lithologic age. Sequence stratigraphic analysis and cross section of Banghan field was revealed. The sidewall core descriptions were used to affirm depositional environment inferred from gamma-ray log trace and seismic geometries. The reservoirs defined using gamma-ray logs are correlated to reveal their vertical and lateral extent. Each reservoir petrophysical property is evaluated. Based on a defined zone of interest, the volume of the reservoirs and hydrocarbon pore volume within it is calculated.
Autorenporträt
Etimita Osuwake Omini is a dynamic geologist with a bachelor degree in Geology from the University of Calabar, Nigeria and a masters degree in petroleum geology from the University of Port Harcourt, Nigeria.This is a publication of my masters degree thesis in geology supervised by Dr. F. T. Beka and examined by Prof C. J. Iwagwu.