petroleum exploration and methods Flashcards
use of satellites or aircraft-based sensor technologies to detect and classify objects
remote sensing
data that uses range of wavelength
spectral data
similar data produced by aerial photraphy
photogeologic data
- gravity used to define regional tectonic regime to prioritize areas for seismic work and to obtain data in inaccessible terrain
- low cost compared to seismic but also yield low res and ambiguous results
gravimetric data
anomalies caused by heterogenous distribution of rocks of different densities
gravity anomalies
strength of the response of the rock to an imposed magnetic field
magnetic susceptibility
- can be collected in areas not easily accessible
- used to separate basin from non basins areas, define the shape of the basin and locate the major teconic features within the basin
magnetic data
the shallowest magnetic rocks in the subsurface are nearest to the magnetometer and will generate the strongest anomalies
yas
3 types of rocks based on magnetivity
- diamagnetic - repulsive force to magnetic field
- paramagnetic - magnetic substances are attracted to mag fields
- ferromagnetic - pronounced magnetic properties
reflection generates seismic waves and measures time taken for the waves to travel from the source, reflect off an interface and be detected by an array of receivers
seismic reflection
body waves
P-waves
surface waves
S-wave
wave emanating from the surface reaches a boundary between two media that have different acoustic independence, some of the energy is reflected back into the upper medium and some may bre fefracted along the interface between two media or to low medium
reflection seismology
ratio of the amplitude of the reflected wave to the incident wave
reflection coefficient
travel time from the surface to reflector and back
two way time
electro-hydraulic vibrator, sweep frequency waveform of several seconds, long sinusoidal wave train may exceed 10 milliseconds, 6-60hz
vibroseis
generates a sharp pulse with a very wide bandwidth, land source, 5-50 lbs charges, drilled holes to base of weathered layer (30-60 ft)
dynamite source
land, electromechanical transducer w/ moving coil
geophones
airgun, bubble pulse successive smaller pulses after main source wavelet, use tuned air guns, water gun source
marine sources
water, pressure sensitive hydrophone, piezoelectric effect produce voltage proportional to seismic pressure wave, +ve voltage output when pressure applied = -ve amplitude
hydrophone
an energy pulse is sent to the subsurface layers and reflected waves are picked by the hydrophones contained in a streamer towed by the survey vessel
Seismic 2D survey
a multi-streamer array is towed by the seismic ship, acquiring overlapping swaths of data over the entire survey area
seismic 3D survey
waves that induces changes in volume and shape of a body
p-waves
waves that induces changes in the shape of the body but not the volume
s-waves
measure of compressability, stress-strain ration for hydrostatic pressure
bulk modulus
rigidity, stress-strain ratio for shear deformation
shear modulus
normal polarity
increase impedance (peak or positive) decrease impedance (trough or negative)
seismic response to impedance contrast accross geological boundaries
reflections
impedance contrast depends on
stacking and migration
cases where 2D data are used
frontier area old pools difficult terrain tie lines testing new seismic acquisition
formation tops or sequence boundaries or unconformities
horizons
displacement along a shear surface
fault
indication of faults
reflection cut-offs
changes in amplitude or reflection character
fault-plane reflectors
linear amplitude anomalies on timesclices
on what direction is best to pick a fault
dip direction