Normal-Fault-Propagation Folding in Mechanically Layered Carbonates and Shale: The Case Against “Fault Drag”
“Fault drag” is often interpreted as the product
of frictional sliding along a fault and progressive tilting of beds with
increased amount of sliding along the fault. We analyze a set of normal faults
with displacement (throw) ranging from 0.5 m to 5 m, and the associated fault-related
folds in mechanically layered upper Cretaceous carbonate and shale in central
Texas. We interpret the set of fault-related folds exposed in outcrop to
represent different stages in the deformation sequence. Fold wavelength is
established early and at small displacement (<0.5 m throw). With increasing
displacement, up to 1 m throw, the monoclinal fold limb steepens, and a
half-meter thick competent bed
within the fold accommodates
bed
-parallel
extension by extension-fracture dilation and slip along
bed
-bound extensional
faults within the fold limb. Further fault displacement, up to 5 m throw,
causes the fold limb to continue stretching and produces boudinage in the most
competent
bed
. Although outer arc extension fracturing is observed in fold
hinges within the competent
bed
, layer extension is present throughout the fold
limb and is concentrated in areas of steep dip rather than being restricted to
high-curvature regions in fold hinges. Clay smear is well developed and a
half-meter thick clay-rich shale is locally thinned to 0.1 m associated with
fault throws of 0.5 to 5 m. We conclude that
bed
tilting and the development of
apparent drag is not the product of frictional sliding but instead folding at
the tip of an upwardly propagating normal fault. Field evidence shows that
fault tip folding in mechanically layered rocks is accommodated by synthetic
dip associated with normal faults and is initiated early in the fault
development history. Synthetic dip associated with normal faults should not be
assumed to be the product of frictional drag, but must be considered in the
context of the mechanical stratigraphy.
AAPG Search and Discovery Article #90142 © 2012 AAPG Annual Convention and Exhibition, April 22-25, 2012, Long Beach, California