Geometry and Fracture Distribution in
Fault
-Propagation
Folds in Nature and Experiments
Judith S. Chester
Fault
-propagation folds in compressional terranes are attractive reservoir
targets, particularly where deformation processes such as fracturing and
faulting enhance reservoir and transport properties. Field examples and
laboratory modeling suggest that fold geometry, fracture distribution, and
propagation of the master
fault
vary with lithologic layering.
Fault
-propagation
folds in the Absaroka thrust sheet, Salt River Range, Wyoming, are characterized
by a complexly folded and faulted sequence overlying imbricate thrust ramps. The
lower Paleozoic section consists of a mechanically anisotropic rock sequence
that has variable bedding thickness and relative ductility. Above thrust ramps,
thick-bedded brittle units shorten by isolated faulting and fracturing. The
faulted and fractured zones are separated by disharmonic folds and zones of
interlayer slip in the thinly bedded units. This geometry suggests that
fault
-propagation folds in mechanically layered rock grow by the linking of
structurally higher isolated faulted segments rather than by the continuous
propagation of the master thrust upsection.
A similar mechanism of fold growth has been observed in experimentally
deformed rock models. Displacement on the master thrust is accommodated in the
overlying sequence by fracturing and faulting in the brittle units and by
disharmonic folding and interlayer slip in the intervening units. In sequences
having a high degree of anisotropy and moderate ductility, a narrow zone of
fracturing and faulting forms. This zone is localized in the fold hinge region
ahead of the propagating master thrust. In sequences having a high degree of
anisotropy and high ductility, intensely fractured zones form on the frontal and
dorsal limbs of the fold, whereas the crest remains relatively undeformed. As
each
fault
-propagation fold grows, the isolated
fault
segments propagate up and
down section, eventua ly coalescing with the master thrust ramp.
AAPG Search and Discovery Article #91030©1988 AAPG Annual Convention, Houston, Texas, 20-23 March 1988.