Geology 5660/6660 Applied Geophysics 19 Feb 2014 © A.R. Lowry 2014 For Fri 21 Feb: Burger 200-253...
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Geology 5660/6660 Applied Geophysics 19 Feb 2014 © A.R. Lowry 2014 Fri 21 Feb: Burger 200-253 (§4.4-4.7) Reflection Data Processing : Migration return reflection energy to its “true” ation on the two-way travel-time image… Depth ration uses velocity structure from NMO correction convert travel time to depth (improving image resol oving e.g. velocity pull-ups/pull-downs) imes additional steps as well: Amplitude adjustments Frequency adjustments mission adjustments Depth Migration he latter especially is important for velocity effe eflection Interpretation collection: Huge quantities of data! Redundancy is ofiling still used for initial reconnaissance, but ustry standard for prospects
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Transcript of Geology 5660/6660 Applied Geophysics 19 Feb 2014 © A.R. Lowry 2014 For Fri 21 Feb: Burger 200-253...
Geology 5660/6660Applied Geophysics
19 Feb 2014
© A.R. Lowry 2014For Fri 21 Feb: Burger 200-253 (§4.4-4.7)
Last Time: Reflection Data Processing• Step IV: Migration return reflection energy to its “true” location on the two-way travel-time image… Depth migration uses velocity structure from NMO correction to convert travel time to depth (improving image resolution; removing e.g. velocity pull-ups/pull-downs)• Sometimes additional steps as well: Amplitude adjustments Frequency adjustments Transmission adjustments Depth Migration (The latter especially is important for velocity effects!)
Seismic Reflection Interpretation• Data collection: Huge quantities of data! Redundancy is key!• 2D profiling still used for initial reconnaissance, but 3D is industry standard for prospects
Haakon Fossen 2010
2D Seismic Data• 2D lines are long profiles that are processed independently
• Generally collected now for regional reconnaissance studies
• Covers large areas and gives an overall picture of the geology
Haakon Fossen 2010
Haakon Fossen 2010
Haakon Fossen 2010
Deep seismic profiling• Imaging depth range from 0-50 km
Strongest & most continuous impedance contrasts below sedimentary cover are lithologic changes ~mid-crust and at the Moho
Haakon Fossen 2010
Other reflectivity within crystalline crust can relate to lithologic changes (e.g. across a low-angle normal fault) but also often represents mineral alignment in ductile shear zones
Haakon Fossen 2010
Haakon Fossen 2010
• Better resolution
• Better positioning
• 3D view options
3-D seismic cubes
Haakon Fossen 2010
3D seismic3D data: • collected by shooting many parallel lines ~25 m apart• migrated together to increase accuracy and to create a coherent data volume (cube) • collected over all offshore oil and gas fields• underpin the geometric understanding of an oil field
Haakon Fossen 2010
Haakon Fossen 2010
Data acquisition
Haakon Fossen 2010
Resolution
• Vertical
• Lateral
Haakon Fossen 2010
Vertical resolution
Relationship between bedthickness and acousticimpedance contrast forseismic resolution of alayer.
Vertical seismic resolution in terms oftuning thickness: When top to baseof a layer is less than 1/4 wavelength,constructive/destructive interferenceresults in apparent single wavelet.
Haakon Fossen 2010
Color convention: Blue for positive amplitude, red for negative…
Haakon Fossen 2010
Haakon Fossen 2010
Haakon Fossen 2010
Haakon Fossen 2010
Lateral positioning
• Choice of migration velocities affects horizontal positioning of signals• Horizontal resolution typically 50-100 m• Serious concern when drilling high-precision wells, e.g. close to faults. • Resolution may depend heavily on pilot wells
Haakon Fossen 2010
Directional drilling/steering technology is another reason for accurate depth migration!
Haakon Fossen 2010
Seismic qualityDepends on:
• Acoustic impedance contrast
• Depth ( frequency)
• Layer thickness ( interference)
• Properties of overlying layers
• Source energy
• Processing parameters
• Acquisition direction
• Instrumentation
