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Abstract:
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A full suite of geophysical logs, including nuclear, electric, acoustic transit-time, acoustic waveform, and acoustic televiewer logs, and high-resolution flowmeter measurements have been used to investigate the lithologic and hydrologic properties of three igneous plutons located on the southern margin of the Canadian shield. Geophysical
logs were used to identify lithologic boundaries, determine the properties of unfractured
granitic or gabbroic rocks, interpret and calibrate the results of surface geophysical
surveys, and characterize permeable fracture zones that could serve as conduits
for fluid migration. Nuclear and acoustic transit-time logs provided good quantitative
correlation with changes in lithology. Electric logs yielded consistent qualitative
correlations, with lower resistivities associated with more mafic lithologies. Lithologic
contacts indentified on logs generally confirmed the results of surface electromagnetic,
seismic, and gravity surveys. All major fracture zones intersected by boreholes were
clearly indicated by the geophysical logs. Electric, epithermal-neutron, and acoustic
transit-time logs gave the most consistent indications of fracturing, but the lithologic
responses associated with some thin mafic intrusions were difficult to distinguish from
possible fractures, and some steeply-dipping fractures were not indicated by conventional
acoustic transit-time logs. Electric and neutron log response is attributed to
the effect of clay minearl alteration products in the vicinity of fractures. This alteration may be indirectly related to permebaility, but no direct relationship between
resistivity or neutron attenuation and permeability appears to exist. Tube-wave attenuation determined from acoustic waveform logs was related to the transmissivity
of equivalent infinite, plane fractures; these results agree qualitatively, and possibly
quantitatively with packer isolation and injection tests if the combined effects of differing scales of investigation and borehole enlargements in fracture zones are taken into account. Tube-wave attenuation in waveform logs also compares well with the permeability distributions determined from tube-wave generation in vertical seismic profiles. Comparison of conventional geophysical logs, acoustic televiewer images of the borehole wall, and fracture frequency distributions measured on core samples indicates
that many fractures are completely sealed and have no effect on log response, whereas
many more apparently sealed fractures have been slightly opened during drilling, and
do provide some log response. High resolution flowmeter meaurements of natural flow
in boreholes and comparison of packer isolation tests with log data indicate that a
relatively few individual fractures often provide a large proportion of fracture zone
transmissivity in the immediate vicinity of the borehole, and that the orientation of
these fractures may not coincide with fracture zone orientation. These results indicate
that the scale problem in relating borehole logs to regional configuration of fracture
flow systems may be the most important consideration in the appplication of geophysical
well logging to the characterization of ground water flow in crystalline rock
bodies. |
