In this study the Cypress Hills aeromagnetic survey of southern Alberta has
been used to deduce if any relationship exists between hydrocarbon pools a
nd the observed total magnetic field. To examine this hypothesis it was nec
essary first to eliminate a large percentage of the signal that is believed
to have originated from other geological, cultural and instrumentation sou
rces. Separation of individual source contributions was defined on the basi
s of amplitude and wave number. The result is a magnetic image where the fe
atures of interest have amplitudes that are predominantly in the single dig
it to sub-nanoTesla range. Several features of the resulting residual magne
tic field seem to be common to a majority of the hydrocarbon pools. These c
ommonalities are: (1) the long axis of the pool appears to be coincident wi
th the strike of the basement-sourced magnetic signal. (2) Hydrocarbon pool
s encompass areas of broad low amplitude magnetic anomalies.(3) Cross-cutti
ng fractures or faulting systems are located within areas of a majority of
hydrocarbon pools. (4) Pools are associated with linear and/or curvilinear
magnetic lineaments a great number of which have topographic expression.