EVOLVING PALEOGEOGRAPHIC INTERPRETATIONS OF THE
HARTFORD AND DEERFIELD RIFT BASINS (NEWARK
SUPERGROUP): AN HISTORIC OVERVIEW
McDONALD, Nicholas G., Dept. of Earth and Environmental
Sciences, Wesleyan University, Middletown, CT 06459
LeTOURNEAU, Peter M., Lamont-Doherty Earth Observatory
of Columbia University, Palisades, NY 10964
In the earliest comprehensive consideration of the depositional
environments of the strata in the various Newark basins, Rogers
(1840) advocated that the sediments were laid down with their present
oblique dip by currents in an extensive "noble" river, which arose in
the mountains of North Carolina and flowed northeastward, eventually
draining into an oceanic estuary near New York City. A similar
scenario was envisioned for the Connecticut Valley Mesozoic rocks by
Mather (1843) and others, except that oceanic currents rather than
fluvial processes were invoked as the depositional agents. At the turn
of the century, championed by Russell (1892) and Emerson (1898),
"Bay of Fundy" analogs for the Connecticut Valley deposits were in
vogue: the sediments presumably accumulating in shallow, broad,
tide-swept estuaries, in which expansive mudflats were subaerially
exposed at low water intervals.
Davis (1898), after nearly 20 years of structural and
physiographic investigations in central Connecticut, hypothesized
sedimentation occurring in an elongate, downwarped trough, bowl-
shaped in cross-section, with no oceanic connections. He postulated
that streams supplied detritus to the slowly sagging basin from both
margins, and that sediments accumulated in near-horizontal layers. In
his model, lacustrine conditions, characterized by fossiliferous black
shales, intermittently prevailed in the central regions of the trough.
Barrell (1915) was a visionary in recognizing that the faults
which bound the eastern edge of the Hartford basin were
syndepositionally active, and exerted a controlling influence on basin
geometry. He theorized deposition in a wedge-shaped trough,
subsiding on the eastern edge, with nearly all of the detritus being
supplied from highlands adjacent to the eastern boundary faults.
Paleoslopes on the basin floor, he suggested, were near horizontal or
gently inclined to the west, and he maintained that the basin once
extended well beyond its present western limit, perhaps even as far as
to be syndepositionally confluent with the Newark basin of New
Jersey. Barrell's model was clearly influenced by the "broad terrane"
hypothesis of Russell (1879), who advocated that the stratigraphically-
similar Hartford and Newark basins are erosional (half graben)
remnants of a once contiguous full graben, postdepositionally isolated
by basement arching in western Connecticut. Barrell's conclusions
and broad terrane principles were endorsed by most subsequent
researchers, including Longwell, Wheeler and Krynine, and received
more recent support from Sanders (1974) and the early studies of
Hubert and his co-workers.
Challenges to broad terrane doctrines in the Hartford basin,
however, were boldly advanced by Klein (1968, 1969), whose
sedimentological data revealed a western provenance and east-dipping
paleoslopes for some deposits in the region, thus rendering persistent
connections with the Newark basin unlikely. Hubert et al. (1978)
however, advocated a modified broad terrane model like that of
Krynine (1950) which connected the Hartford Basin with the
Pomperaug Basin of western Connecticut based on localized
southwest paleocurrent trends in the upper Triassic strata, assumed
westerly paleoslopes on Jurassic lake floors, and the "likely" extension
of an East Berlin Formation perennial lake to the Pomperaug Basin.
Studies of the Jurassic strata of the Hartford basin by
LeTourneau (1985), LeTourneau and McDonald, (1985); McDonald
and LeTourneau (1988, 1990) using paleocurrents, sediment
provenance, facies analysis, stratal geometry, modeled configuration
of the hinged and faulted basin margins, and basalt flow directions
(Ellefsen and Rydel, 1985), proposed an asymmetrically subsiding
basin that was deepest adjacent to the eastern border faults. In this
isolated basin model, east-dipping paleoslopes prevail on the broad,
western, hinged-margin side of the basin, and small, steep drainages
flow west from the narrow eastern footwall margin into the adjacent
depocenter. Hettangian-age fossiliferous black shale units which
invariably thicken toward the basin margin rather than toward basin
center provide a demonstrative argument for basin isolation. Hubert,
et al. (1992), armed with additional petrographic data indicating the
prevalence of western (hinged-margin) sediment sources, rejected the
earlier "modified-broad terrane" positions of Hubert et al. (1978) and
Weddle and Hubert (1983) and supported the isolated half graben
model advocated by LeTourneau and McDonald. McHone (1996),
however, resurrects the possibility of basin interconnections during the
Triassic, and provides compelling evidence for a broad terrane Jurassic
flood basalt province which may have extended over much of
northeastern North America.
The isolated basin model presented above is supported by recent
work on the structural geology of modern and ancient continental rift
basins. Models based on sedimentary facies analysis suggest a
tectonic framework common to extended terranes (Kusznir and Egan,
1989; Kusznir et al. 1995; Rosendahl et al., 1986; Rosendahl, 1987;
Schlische and Anders, 1996; Scholtz and Rosendahl, 1990).
Asymmetric half graben are the most common form of rift basins.
Due to differential isostatic loading, the footwall of the master border
fault system undergoes profound uplift during extension, resulting in
small, steep catchments on the faulted margin. The basin depocenter
is skewed toward the faulted margin. The broad area of the hinged or
platform margin dips shallowly toward the faulted margin and
contains major inflowing rivers. Most basin-filling sediment is
derived from hanging wall and axial sediment sources; footwall
sources are only of local importance. Pre-rift drainages may be
captured or breach the footwall (Johnson, Wells and Scholtz, 1995;
Smoot 1995). Half-graben may be linked perpendicular to the main
extension direction, as seen in the modern East African rift basins, the
Newark-Gettysburg-Culpeper basin complex, and the Hartford-
Deerfield complex. Studies of the varied structural and depositional
histories of modern rift basins may ultimately prove the fallibility of
simplistic models for the paleogeography of the Newark basins.
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