Abstract
We study the influence of composition and shape of massive sulfide
ore deposits hosted in crystalline rocks on the full scattered wavefield
through a series of numerical modelling experiments based on the
3-D elastic Finite Difference (FD) method. Ores consisting of the
ned-member sulfide minerals pyrite, sphalerite and galena, which
span the full range of observed velocities and densities in ore rocks,
as well as gabbro inclusions are investigated for six different shapes
which represent the complex morphologies often observed for ore deposits.
3-D FD modelling revealed that large ore deposits lead to a strong
and complex scattering response which is dominated by shear wave
events. Scattering from massive sulfides cannot be described accurately
by the widely used Born approximation. The directional distribution
of the scattered wavefield is mainly controlled by the shape of the
ore. The directivity imposed by shape is a first-order characteristic
of the scattered wavefield, whereas composition effects are of secondary
importance. Amplitude focussing caused by the shape of the deposit
may lead to very strong amplitude versus offset/azimuth trends. Therefore,
the interpretation of amplitude versus offset/azimuth variations
along scattering hyperbolas is highly ambiguous without detailed
a priori knowledge of shape. If observed, they may serve as a diagnostic
tool to classify the composition of the scattering object.
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