HYDROGEOLOGIC CHARACTERIZATION OF FRACTURED
SEDIMENTARY BEDROCK IN THE HARTFORD RIFT BASIN
USING BOREHOLE-GEOPHYSICAL TECHNIQUES
STONE, Janet Radway, STARN, J. Jeffrey, MELVIN,
Robert L., U. S. Geological Survey, 450 Main St.,
Hartford CT 06103
Recent investigations were conducted by the U. S. Geological Survey
at two ground-water contamination sites, one in the Portland
Formation in Durham, Connecticut (Melvin and others, 1995) and one
in the New Haven Arkose in Cheshire, Connecticut (Stone and others,
1996). Borehole-geophysical logging, coupled with geologic analysis
and hydraulic testing, reveal that bedding-parallel partings and
fracture planes provide the major pathways for ground-water flow in
the sedimentary bedrock of the Hartford Basin. The studies also
indicate that only a small number of these geologic features are
hydraulically significant. Ground water moves along some
subhorizontal, bed-parallel features such as bedding-plane partings at
the base of coarse channel-sandstone units and fissile zones within
finer-grained mudstone units, and moves across bedding planes along
open, high-angle fractures. The direction of ground-water flow and
contaminant transport within the bedrock is greatly affected by the
resultant geometry of intersecting bedding planes and fracture planes.
Borehole-geophysical logs used to interpret lithology, fracture
type and fracture orientation include natural gamma, formational
resistivity, caliper, TV camera, and acoustic-televiewer. At the
Cheshire site, in the New Haven Arkose, logs showed a strong inverse
correlation between gamma and formational resistivity, and
comparison to rock core indicated that gamma values were a good
indicator of textural variation between beds. In the Portland
Formation, in the Durham Center area, the presence of higher amounts
of K-feldspar in many textural units, precluded the use of gamma logs
as an indicator of grain-size. In the boreholes at Durham, the highest
gamma peaks were commonly present where high-angle fractures
intersect the borehole wall. At both localities, the downhole TV log
provided important lithologic and fracture information, but acoustic
televiewer logging was required to determine the orientation of
fractures and bedding. Borehole-geophysical logs used to identify
significant water-bearing zones in bedrock wells include fluid
conductivity, fluid temperature and heat-pulse flowmeter. Flowmeter
logging was done under natural, nonstressed conditions, and single-
and multi-well logging was also done under pumping conditions to
interpret hydraulic connectivity of fractures.
At both Cheshire and Durham, rock units strike nearly N-S and dip
gently eastward at <5o to 20o. In Cheshire, fracture orientations were
measured in outcrop and in four bedrock wells. The dominant fracture
set strikes NNE and dips steeply WNW, perpendicular to bedding; the
paleovertical orientation appears to be a result of syndepositional, rift-
basin extension. These high-angle fractures have limited vertical
extent and occur mostly in the more competent channel-sandstone
units, extending only locally into the mudstone units. In Durham,
high-angle fractures measured in 13 bedrock wells strike dominantly
NE and dip both NW and SE. Fracturing at this location is associated
with postdepositional faulting; individual high-angle fractures have
greater vertical extent and are more significant hydraulically than are
bed-parallel features. The investigation strongly indicates that a NE-
striking, NW-dipping normal fault (shown by mapped offsets in
Hampden Basalt to the west on geologic maps) extends into the
Portland Formation through the Durham Center area, where we refer
to it as the Ball Brook Fault. Yields of bedrock wells penetrating the
fault zone are anomalously high.
Melvin, R. L., Stone, J. R., Craft, P. A., Lane, J. W., and Davies, B. S., 1995,
Geohydrology and water quality of the Durham Center area, Durham,
Connecticut: U.S. Geological Survey Water-Resources Investigations Report
94-4237, 97 p.
Stone, J. R. , Barlow, P. M., and Starn, J. J., 1996, Geohydrology and conceptual
model of a ground-water flow system near a Superfund site in Cheshire,
Connecticut: U. S. Geological Survey Open-File Report 96-162, 88 p.
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