Numerical Modeling of Salt Tectonics on Passive Continental Margins: Preliminary Assessment of the Effects of Sediment Loading, Buoyancy, Margin Tilt, and Isostasy
Steven Ings1,
Christopher Beaumont2, and Lykke Gemmer2
1Department
of Earth Sciences,
sings@dal.ca
2Department
of Oceanography,
Salt tectonics in passive continental
margin settings is investigated using a 2D vertical cross-sectional finite
element numerical model of frictional-plastic sedimentary overburden overlying
a linear viscous salt layer. We present
preliminary results concerning the effects of sediment progradation
over the salt, buoyancy driven flow owing to density contrast between the
sediment and salt, regional tilt of the salt layer, and local isostatic adjustment of the system. Sediment progradation
causes a differential load on the underlying salt, which may lead to
instability of the system with landward extension accommodated by seaward distal
contraction. Slow progradation
(Vsp
= 0.5 cm/yr) of aggrading sediments gives a diachronous
evolution comprising four main phases: 1) initiation of salt channel flow and
the formation of minibasins and associated diapirs; 2) onset of listric
normal growth faulting and extension of the sedimentary overburden; 3) large
scale evacuation of the salt, formation of pre-rafts and rafts, and inversion
of the minibasins; 4) formation of a contractional allochthonous salt nappe that overthrusts the
depositional limit of the salt.
Buoyancy effects are investigated
using models with density contrasts between overburden and sediment of 0, 100
and 400 kg/m3. Although the lateral flow driven by differential
loading dominates in all cases, the form of the minibasins,
the overall salt evacuation, and style of diapirism
are sensitive to buoyancy forces, with the large density contrast producing the
most developed diapiric and minibasin
structures.
A regional basinward
tilt of 0.2° (of the type that may be produced by thermal contraction of the
rifted margin) enhances and accelerates the overall seaward flow of the
unstable slope region of the model leading to much earlier overthrusting
of the distal depositional limit of the salt.
The added downslope gravitational component
also modifies the style of the minibasins by
enhancing the horizontal channel flow by comparison with the vertical buoyancy
driven flow. This reduces the apparent
efficiency of diapirism.
Local isostatic
adjustment, owing to overburden and water loading, introduces a landward tilt
of the system, thereby requiring salt to flow updip
against gravity during evacuation. Isostasy also changes the overburden geometry and,
therefore, modifies the stability and flow velocity of the extending overburden
through the increased strength of the isostatically
thickened proximal overburden, and through the modified differential pressure
acting on the salt under these circumstances.
The seaward flow of the unstable slope region is slower for the same
overburden progradation velocity, more salt remains beneath
the shelf as rollers and pillows during evacuation, counter-regional faults are
more pronounced, and the allochthonous salt nappe progressively climbs above the isostatically
adjusting sediments as it overthrusts.