Deep burial diagenesis and reservoir quality along the eastern flank of the Viking Graben. Evidence for illitization and quartz cementation after hydrocarbon emplacement

Clay Minerals

Volumn 35, Issue 1, 2000, Pages 227-237

  Midtbo, R E A ^a   Rykkje, J M ^a   Ramm, M ^a  

^a STATOIL   (Norway)

Author keywords

Burial diagenesis; Hydrocarbon emplacement; Reservoir quality; Tarbert Formation; Viking Graben

Indexed keywords

BURIAL DIAGENESIS; CEMENTATION; HYDROCARBON RESERVOIR; ILLITIZATION; QUARTZ; RESERVOIR CHARACTERIZATION;

NORTH SEA; VIKING GRABEN;

CHEMICAL ANALYSIS; COMPOSITION; FELDSPAR; HYDROCARBONS; KAOLIN; PETROLEUM RESERVOIRS; PHASE TRANSITIONS; POROSITY;

DEEP BURIAL DIAGENESIS; HYDROCARBON EMPLACEMENT; RESERVOIR QUALITY; TARBERT FORMATION; VIKING GRABEN;

QUARTZ;

EID: 0033626689     PISSN: 00098558     EISSN: None     Source Type: Journal    
DOI: 10.1180/000985500546602     Document Type: Conference Paper

References (12)

1. Combined use of confocal laser scanning microscopy and PVT simulation for estimating the composition and physical properties of petroleum in fluid inclusions
2. Sandstone diagenesis and porosity modification during basin evolution
3. Diagenetic processes in the Brent Group (Middle Jurassic) reservoirs of the North Sea - an overview
4. Diagenesis and reservoir properties of Jurassic sandstones from the Haltenbanken area, offshore Mid Norway
5. Relationship between diagenesis and reservoir quality in sandstones of the Garn Formation. Haltenbanken, Mid-Norwegian continental shelf
6. Factors controlling permeability variation of the Garn Formation in Trestakk field, Norwegian continental shelf
7. Formation of diagenetic illite in sandstones of the Garn formation, Haltenbanken area, Mid Norwegian continental shelf
8. Compaction of lithic sands: Experimental results and applications
9. Reservoir quality and burial diagenesis in the Statfjord Formation, North Sea
10. Geologic pressure determinations from fluid inclusion studies
11. Temperatures of quartz cementation in Jurassic sandstones from the Norwegian continental shelf - evidence from fluid inclusions