Interpreted ranges of effective fracture apertures.

Slides:



Advertisements
Similar presentations
Fracture Properties Needed
Advertisements

Well logging course for fourth year
Fracture Spacing in Miss. Madison Ls
Some basic Log interpretation
Use of Geologic Maps and Structural Geology to locate an oil well.
Petroleum System – Source Rock
68th EAGE Conference and Exhibition, Vienna 1 Impact of Time Lapse Processing on 4D Simultaneous Inversion The Marlim Field Case Study C. Reiser * 1, E.
Department of Geology and Geological Engineering
STRUCTURAL GEOLOGY LAB. STEREOGRAPHIC PROJECTION Dr. Masdouq Al-Taj
R. G. Pratt1, L. Sirgue2, B. Hornby2, J. Wolfe3
On the equality of resistivity fractal dimension and geometric relaxation time fractal dimension of induced polarization for characterizing Shajara Reservoirs.
Quantitative Analysis of Older Logs for Porosity and Permeability; West Flank Reservoirs, Lake Maracaibo, Venezuela E.R. (Ross) Crain* (Spectrum 2000.
Maps of eroded thicknesses of Triassic, Jurassic and Cretaceous sediments: (a) eroded thickness of the Triassic; (b) Lower and Middle Jurassic; (c) Upper.
by A. Belaidi, D. A. Bonter, C. Slightam, and R. C. Trice
Merged map showing the Late Jurassic tectonic framework of the Danish Central Graben after Ineson et al. Merged map showing the Late Jurassic tectonic.
Measured and modelled vitrinite reflectance and present-day temperature data in a selection of wells in the study area: (a, b) modelled vitrinite reflectance.
Main structural features of the East Siberian Sea Shelf.
Simplified stratigraphic chart showing the age of the main depth maps used in the 3D model (dashed lines). Simplified stratigraphic chart showing the age.
Alexey Stovas NTNU, Trondheim 2005
Disturbance of seafloor sediments on high-latitude shelves.
Calculated maturity (vitrinite reflectance values; Sweeney & Burnham 1990) at the top of the Hot Shale unit over four time steps: (a) modelled maturity.
Main sedimentary basins of the Siberian Arctic Shelf (modified from Grantz et al. 2009). Main sedimentary basins of the Siberian Arctic Shelf (modified.
The burial history of three 1D extractions from the 3D model: (a) 1D burial history at the location of well C-16-1 in the Central Graben; (b) of well B-11-2.
Log data from 205/21a-6 across an interval of Fractured Basement and an interval of Fault Zone. Log data from 205/21a-6 across an interval of Fractured.
Example 1 of SPE : Simultaneous versus Well-by-Well Optimization
Chapter 1 Introduction to the geology of Myanmar
Schematic overview of depositional environments occurring in the terrestrial and marine realm which are mentioned in the text. Schematic overview of depositional.
Merged map showing the Late Jurassic tectonic framework of the Danish Central Graben after Ineson et al. Merged map showing the Late Jurassic tectonic.
(a) Location map and the subdivision (northern, southern, central) of the study area. (a) Location map and the subdivision (northern, southern, central)
Summary of bulk porosity measurements and bulk porosity interpretation from LWD density neutron data recorded in the horizontal well. Summary of bulk porosity.
South China Sea crustal thickness and oceanic lithosphere distribution from satellite gravity inversion by Simon Gozzard, Nick Kusznir, Dieter Franke,
Newbury slope: (a) slope cross-section and soil water retention and hydraulic conductivity function properties for the modelled London Clay; (b) history.
The Petroleum Geology of NW Europe: 50 years of learning – a platform for present value and future success. An overview by Bruce Levell, and Mike Bowman.
Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Posidonia Shale unit over four time steps: (a) modelled maturity.
Simplified cross-section illustrating internal structure and inferred stratigraphy of the South Chukchi and North Chukchi basins. Simplified cross-section.
Geometry and key elements of the Central Andaman Basin and East Andaman Basin. Geometry and key elements of the Central Andaman Basin and East Andaman.
Summary diagram of the Upstream Exploration and Production Value Chain illustrating the range of uncertainty and value creation from access to cessation.
The three fracture end members (microfractures, joints and seismically identified faults) that comprise the Lancaster conceptual model. The three fracture.
The glaciated trough of the Gasterntal, looking up-valley from the Stock hill; the 1908 tunnel breakthrough created a valley-floor sinkhole in the woodland.
(a) Map of the Isle of Skye (Scotland), with a box denoting Brothers’ Point (Rubha nam Brathairean), where the two theropod teeth described here (NMS G
(a) Outcrop evidence of overpressure along the Sagaing Fault: sandstones injected into a bedded Miocene sandstone. (a) Outcrop evidence of overpressure.
Oil saturation through four steps of simulated production showing a comparison of how host rock models with high (1000 mD) and low (150 mD) permeabilities.
Map showing approximate limits of Northern Hemisphere ice sheets at the present day and during the Last Glacial Maximum (LGM). Map showing approximate.
Sensitivity of crustal thickness and continental lithosphere thinning determined from gravity inversion to sediment thickness used in the gravity inversion.
Pressure ridge west of the Yangon–Naypyidaw–Mandalay Expressway, south of Naypyidaw ( ° N, ° E): (a) view of the ridge; (b) more coherent.
Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Namurian–Visean unit over four time steps: (a) Late Carboniferous;
Schematic cross-section from the eastern Alcock Rise across the East Andaman Basin, SE offshore Myanmar. Schematic cross-section from the eastern Alcock.
Data-driven workflow to obtain dynamic fluid-flow model and structural data from acquired drone images. Data-driven workflow to obtain dynamic fluid-flow.
Comparison of graphic log systems illustrating the difference in geological message between (a) use of basic symbols used with ‘artistic flexibility’ and.
Approximately 2 m diameter shaft exposed at the site of the Nottingham Business Park near Strelley. Approximately 2 m diameter shaft exposed at the site.
Orientation of SHmax over the non-gas-bearing structure in Quadrant 43, derived from analysis of borehole breakouts in well 43/12-1. Orientation of SHmax.
by M. Baba, J. Parnell, S. Bowden, J. Armstrong, M. Perez, and X. Wang
Pressure derivative plot from 205/21a-6 DST data.
Knowledge v. solution skills matrix from Roberts (1963) as reported in Stapledon (1996). Knowledge v. solution skills matrix from Roberts (1963) as reported.
Rafts of chalk emplaced within shallow marine sands and gravels of the Wroxham Crag Formation, exposed in the cliff face at Sidestrand, Norfolk; the upper.
The composite BGR seismic reflection line (line 1 in Fig
The ‘Oil Patch Warrior’, a statue in the Dukes Wood Nature Reserve commemorating the 44 roughnecks who arrived from Oklahoma in 1942 to develop the Dukes.
Schematic cross-section for the Outer Wash, showing the ground conditions interpreted by the British Geological Survey (1991). tk, Undivided Mesozoic Strata.
Russia, FSU and the Circum-Arctic: ‘the final frontier’
(a) Southern Scotland and northern England coalfield exposure and locality of the Greenburn surface mine and (b) regional mineral resource geology of the.
Map showing the geographical locations of the contributions to the Atlas of Submarine Glacial Landforms (yellow dots). Map showing the geographical locations.
NW–SE section across Figure 2 showing the regional dip (exaggerated) of the post-Palaeozoic strata and the NW-facing scarp slopes of the Permian strata.
Summary geology of the North Sea and broader region illustrating the principal reservoir and source systems, and showing the range of papers covered in.
(a) Location map and the subdivision (northern, southern, central) of the study area. (a) Location map and the subdivision (northern, southern, central)
Introducing the Energy Geoscience Series
Ferric iron content of garnet and spinel from mantle rocks plotted as a function of the calculated log fO2 using equations (9)–(11). Ferric iron content.
Extract from the Intersect full-field simulation model exhibiting a pressure drawdown snapshot over a particular reservoir depth in relation to the horizontal.
Boundary conditions for the basin modelling include: (a) the history of palaeowater depth (PWD) and (b) sediment–water interface temperature (SWIT) that.
Transformation ratio evolution of the Hot Shale layer in the John Graben extracted from the 3D basin model for three different reaction kinetics after.
Crustal cross-sections with Moho from gravity-anomaly inversion along line 1. Crustal cross-sections with Moho from gravity-anomaly inversion along line.
Presentation transcript:

Interpreted ranges of effective fracture apertures. Interpreted ranges of effective fracture apertures. Fractures (TS) represent fracture aperture ranges estimated from thin-section measurements. Joints reflect estimates of joint aperture ranges from manual estimates of borehole image logs corrected for fracture dip and borehole attitude. Veins (TS) represent widths of veins measured from thin section; and vein image logs represent vein widths estimated from FMI images. Note that veins are mineral-filled fractures and therefore do not contribute to reservoir porosity or permeability. The range of estimated fracture apertures is consistent with extremely high fracture permeability (Kair) and zero immobile water saturation (Sw) (Aguilera 1999). A. Belaidi et al. Petroleum Geology Conference series 2018;8:385-398 © 2018 The Author(s). Published by the Geological Society, London