Integrating Basin and PVT Modeling to Improve Prediction of Fluid Compositional Evolution in High-Pressure/High-Temperature (HP/HT) Settings of the Central Graben, North Sea
Neumann, Volkmar1,
Rolando Di Primio1, Robert Ondrak1,
Robert Lippmann2, Reinhard Gaupp2,
Brian Horsfield1 (1) Geoforschungszentrum,
We analyzed the
compositional evolution of hydrocarbon fluids on a basin-wide scale using fluid
samples and core extracts from high pressure-high temperature (HPHT) reservoirs
in the British and Norwegian Sector of the Central Graben.
The results were integrated in 3D-basin modeling in order to reconstruct
burial, temperature and HC-fluid flow history of the study area. The Mesozoic
reservoirs are situated at 4-5 km depth reaching temperatures of up to 192°C
and pressures of up to 80 MPa. Reservoir fluids are
gas condensates and black oils. A compositional kinetic model calibrated with
PVT-data from reservoir fluids was been used in the 3D-models to determine
timing of first hydrocarbon fluid emplacement, and fluid phase
evolution in the
reservoir. Results indicate a significant difference in the charge histories
of both areas. The reservoir in the
phase
. With
increasing burial, additional kitchen areas became mature and contributed to
the HC-fluid in the reservoir, increasing the liquid content as indicated by
decreasing GORs. The fluid
phase
became undersaturated with onset of overpressure during Late
Cretaceous. Present composition and
phase
behavior are predicted correctly by
the model. Fluid emplacement in the Norwegian study area occurred during Late
Cretaceous to Early Paleocene as saturated black oil. These fluids increased in
GOR during further source rock maturation and by inreservoir
oil to gas cracking driven by reservoir burial. Present undersaturated
gas-conden-sate compositions encountered are also
correctly reproduced by the
phase
modeling results.